From Wikipedia, the free encyclopedia
Rain is liquid
precipitation, as opposed
to other kinds of precipitation such as
snow,
hail and
sleet.
.^ Contrary to what is suggested in the popular media, it is water that is the most important greenhouse gas in Earth's atmosphere, not the small amount of demonized CO 2 ...
.^ More over, a consensus among the countries, which are affected by the climate change, becomes essential for a pragmatic culmination of the negotiation process that is leading to the final round of climate change negotiation in the forthcoming Copenhagen summit .
Virga is precipitation that begins falling to the
earth but evaporates before reaching the surface; it is one of the
ways air can become saturated. Precipitation forms via collision
with other rain drops or ice crystals within a
cloud.
.^ It was not like our soft English rain that drops gently on the earth; it was unmerciful and somehow terrible; you felt in it the malignancy of the primitive powers of nature.
Unpolluted rainfall has a
pH
level of 5.2, making it slightly acidic.
Moisture overriding associated with
weather fronts is an
overall major method of rain production. If enough moisture and
upward motion is present, precipitation falls from convective
clouds such as
cumulonimbus and can organize into narrow
rainbands. In mountainous areas, heavy
precipitation is possible where upslope flow is maximized within
windward
sides of the terrain at elevation.
.^ But this episode is generating more heat than light and is likely to lead to more public confusion over the causes of climate change .
The movement of the
monsoon trough,
or
intertropical convergence zone, brings
rainy seasons to
savannah
climes.
.^ Wind, water and solar technologies can provide 100 % of the world ' s energy by 2030, using only technologies that work or are close to working today on a large scale ...
The
METAR code for rain is
RA.
Rainfall is measured through the use of
rain gages. Rainfall
amounts are estimated actively by
weather radar and passively by
weather
satellites.
The
urban
heat island effect leads to increased rainfall, both in amounts
and intensity, downwind of cities.
.^ Volcanoes cause global warming or cause global cooling?
^ When the circulation changed so that the North got cooler, the South got warmer, and vice versa — a far cry from the current warming all around the globe.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Peru's mountain people 'face extinction because of increasingly cold conditions' -- cold blamed on global warming!?
.^ Black carbon wasn't even listed as a warming agent in the most recent report from the IPCC, but it may be responsible for almost one fifth of the planet ' s warming ...
The globally-averaged annual
precipitation is 990 millimetres (39 in).
.^ In a new report, scientists used seven different climate models to assess the influence of human induced land cover change on climate.
^ Obama's deal 'nothing short of climate change skepticism in action' -- 'Obama has eliminated any difference between him and Bush' .
Australia is the
Earth's driest continent. Rain is also known or suspected on other
worlds. On
Titan,
Saturn's largest moon,
infrequent
methane rain is
thought to carve the moon's numerous surface channels. On
Venus,
sulfuric acid virga evaporates 25 km from the surface.
There is likely to be rain of various compositions in the upper
atmospheres of the
gas
giants, as well as precipitation of liquid
neon and
helium in the deep atmospheres.
How
air becomes saturated
Air contains water vapour, measured in grams of water per
kilogram of dry air (g/kg),
[1] but
most commonly reported as a
relative humidity. How much water
vapour a parcel of air can contain before it becomes saturated
(100% relative humidity) depends on its temperature.
.^ They noted that a warmer ocean would tend to evaporate more of its carbon dioxide gas ( CO 2 ) and also water vapor into the air, whereas a colder ocean would tend to absorb both gases.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
Therefore, one way to saturate a parcel of air is to
cool it. The
dew point
is the temperature to which a parcel must be cooled in order to
become saturated.
[2] Water
vapour normally begins to condense on
condensation nuclei such as
dust, ice, and salt in order to form clouds. An elevated portion of
a frontal zone forces broad areas of lift, which form clouds decks
such as
altostratus or
cirrostratus.
.^ Applications of the Precautionary Principle tend to rest on the premise that global warming is more dangerous, or more to be feared, than global cooling.
It can also form due to the
lifting of
advection fog during
breezy conditions.
[3]
There are four main mechanisms for cooling the air to its dew
point: adiabatic cooling, conductive cooling, radiational cooling,
and evaporative cooling.
Adiabatic
cooling occurs when air rises and expands.
[4] The air
can rise due to
convection, large-scale atmospheric motions,
or a physical barrier such as a mountain (
orographic
lift).
.^ UK Hadley Center: 'I don't think anybody is surprised that we're going to get one model that suggests it's going to cool and another that suggests it's going to warm' .
^ Water takes longer to heat up and does not cool off as easily as land ...
Radiational cooling occurs due
to the emission of
infrared radiation, either by the air
or by the surface underneath.
[6]
Evaporative cooling occurs when moisture is added to the air
through evaporation, which forces the air temperature to cool to
its
wet-bulb temperature, or until it
reaches saturation.
[7]
.^ They saw that the vast mass of water that gradually creeps northward near the surface of the Atlantic is as important in carrying heat as the familiar and visible Gulf Stream.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Perhaps in earlier geological eras when the poles had been warmer, salty ocean waters had plunged in the tropics and come up near the poles.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Arctic melting will release huge quantities of fresh water flowing into the Arctic Ocean.
[13]
Formation
Raindrops are not tear-shaped. Very small raindrops are nearly
spherical As raindrops increase in size, they become flattened at
the bottom due to air resistance. The largest raindrops split into
smaller raindrops due to air resistance.
Coalescence occurs when water
droplets fuse to create larger water droplets, or when water
droplets freeze onto an ice crystal, which is known as the
Bergeron
process. Air resistance typically causes the water droplets in
a cloud to remain stationary. When air turbulence occurs, water
droplets collide, producing larger droplets. As these larger water
droplets descend, coalescence continues, so that drops become heavy
enough to overcome air resistance and fall as rain.
.^ The Paleocene Eocene Thermal Maximum is one of the most dramatic bouts of global warming known to science .
[14] In
clouds below freezing, when ice crystals gain enough mass they
begin to fall.
.^ Perhaps it was a slow sloshing of water masses that had made temperatures there, more than in many other regions, rise so noticeably until the 1940s, then dip until the 1970s ( link from above ).- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
This process is temperature dependent, as supercooled water
droplets only exist in a cloud that is below freezing.
.^ Why was there an ice age in the Late Ordovician Period, when greenhouse gas levels were nearly 12 times higher then they are today ?
^ The models gave reasonably correct pictures of how sea temperatures changed when perturbed by a great volcanic eruption or even an ice age.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ You know what these natives are, they`re quite capable of storing it where the rain will beat in on it all the time."
[15]
Raindrops have sizes ranging from 0.1 millimetres
(0.0039 in) to 9 millimetres (0.35 in) mean
diameter, above which they tend to break up. Smaller drops are
called cloud droplets, and their shape is spherical. As a raindrop
increases in size, its shape becomes more oblate, with its largest
cross-section facing the oncoming airflow.
.^ It was not like our soft English rain that drops gently on the earth; it was unmerciful and somehow terrible; you felt in it the malignancy of the primitive powers of nature.
[16]
Contrary to popular belief, their shape does not resemble a
teardrop.
[17] The
biggest raindrops on Earth were recorded over
Brazil and the
Marshall Islands in 2004 — some
of them were as large as 10 mm. The large size is explained by
condensation on large
smoke
particles or by collisions between drops in small regions with
particularly high content of liquid water.
[18]
Intensity and duration of rainfall are usually inversely
related, i.e., high intensity storms are likely to be of short
duration and low intensity storms can have a long duration.
[19][20] Rain
drops associated with melting hail tend to be larger than other
rain drops.
[21]
Raindrops impact at their
terminal velocity, which is greater
for larger drops due to their larger mass. At sea level and without
wind, 0.5 mm
drizzle
impacts at about 2 m/s, while large 5 mm drops impact at
around 9 m/s.
[22] The
sound of
raindrops hitting water is caused by bubbles of air oscillating
underwater. The METAR code for rain is RA, while the coding for
rain showers is SHRA.
[23]
Acidity
Rainfall with low
pH levels, or
acid rain, is also a
frequent risk produced by lightning within thunderstorms.
.^ Carbon-dioxide emissions are turning the waters of the Arctic Ocean into acid at an unprecedented rate, scientists have discovered.
^ No Rise of Atmospheric Carbon Dioxide Fraction in Past 160 Years, New Research Finds .
“Clean” or unpolluted rain has a slightly
acidic pH of about
.^ They noted that a warmer ocean would tend to evaporate more of its carbon dioxide gas ( CO 2 ) and also water vapor into the air, whereas a colder ocean would tend to absorb both gases.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Other groups using carbon-14 data agreed that on average the ocean waters took at least several hundred years to turn over.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Carbon-dioxide emissions are turning the waters of the Arctic Ocean into acid at an unprecedented rate, scientists have discovered.
[24] Nitrous oxide
present during thunderstorm phenomena,
[25]
caused by the splitting of nitrogen molecules, can result in the
production of acid rain, if nitrous oxide forms compounds with the
water molecules in precipitation, thus creating acid rain. Acid
rain can damage buildings and other external structures.
.^ The acid might eventually dissolve the calcium-carbonate shells of plankton and other creatures important in marine food chains, with uncertain effects on seawater chemistry.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
[27]
Causes
Frontal
activity
Main article:
Weather fronts
Stratiform or dynamic precipitation occurs as a consequence of
slow ascent of air in
synoptic systems (on the
order of cm/s), such as over surface
cold fronts, and over and ahead of
warm fronts. Similar
ascent is seen around
tropical cyclones outside of the
eyewall, and in
comma-head precipitation patterns around
mid-latitude cyclones.
[28]
A wide variety of weather can be found along an occluded front,
with thunderstorms possible, but usually their passage is
associated with a drying of the air mass. Occluded fronts usually
form around mature low-pressure areas.
[29]
Convection
Convective rain, or showery precipitation,
occurs from convective clouds, e.g.,
cumulonimbus or
cumulus congestus. It falls as showers with
rapidly changing intensity. Convective precipitation falls over a
certain area for a relatively short time, as convective clouds have
limited horizontal extent. Most precipitation in the
tropics appears to be
convective; however, it has been suggested that stratiform
precipitation also occurs.
[28][30] Graupel and
hail indicate convection.
[31] In
mid-latitudes, convective precipitation is intermittent and often
associated with baroclinic boundaries such as
cold fronts,
squall lines, and warm fronts.
[32]
Orographic
effects
Orographic precipitation occurs on the
windward side of mountains
and is caused by the rising air motion of a large-scale flow of
moist air across the mountain ridge, resulting in
adiabatic cooling and condensation.
.^ Climate Scare Fading: 'More Americans believe in haunted houses than man-made global warming' - 37% vs. .
^ Provision 'declares a climate emergency if world greenhouse gas levels climb above 450 parts per million' .
^ Warming Establishment Crumbles: More than 140 scientists challenge UN's climate claims in open letter .
Moisture is removed by orographic lift, leaving drier air (see
katabatic wind)
on the descending and generally warming, leeward side where a
rain shadow is
observed.
[13]
.^ Ice-cores reveal that Mount Kilimanjaro has been covered in glaciers for almost 12,000 years.
[33]
Systems known as
Kona
storms affect the state with heavy rains between October and
April.
[34]
Local climates vary considerably on each island due to their
topography, divisible into windward (
Koʻolau)
and leeward (
Kona) regions based upon location relative to
the higher mountains. Windward sides face the east to northeast
trade
winds and receive much more rainfall; leeward sides are drier
and sunnier, with less rain and less cloud cover.
[35]
Within the
tropics
Rainfall distribution by month in
Cairns showing the extent of the wet season
at that location
.^ One more headache: When the drop down menues partially cover an icon, they erase that portion of the icon.- mozdev.org - themes: themes/rain 16 January 2010 19:19 UTC themes.mozdev.org [Source type: General]
^ Submitted by: Dan Thursday September 18th 2003 To answer my own question @77, I tried one more time and got in with no problem.- mozdev.org - themes: themes/rain 16 January 2010 19:19 UTC themes.mozdev.org [Source type: General]
^ One of the largest glaciers in Antarctica is now thinning four times faster than it was ten years ago.
[39] The
term
green season is also sometimes used as a
euphemism by tourist
authorities.
[40] Areas
with wet seasons are dispersed across portions of the
tropics and
subtropics.
[41] Savanna climates and areas with
monsoon regimes have wet
summers and dry winters. Tropical rainforests technically do not
have dry or wet seasons, since their rainfall is equally
distributed through the year.
[42]
Some areas with pronounced rainy seasons will see a break in
rainfall mid-season when the
intertropical convergence zone or
monsoon trough
move poleward of their location during the middle of the warm
season.
[19]
When the wet season occurs during the warm season, or
summer, rain falls mainly during
the late afternoon and early evening hours. The wet season is a
time when
air quality improves,
[43]
freshwater quality improves,
[44][45] and
vegetation grows significantly.
Tropical cyclones, a source of very heavy rainfall, consist of
large air masses several hundred miles across with low pressure at
the centre and with winds blowing inward towards the centre in
either a clockwise direction (southern hemisphere) or
counterclockwise (northern hemisphere).
[46]
.^ But I think, sidebar tab headers and browser tabs are too high, they take up too much of window space.- mozdev.org - themes: themes/rain 16 January 2010 19:19 UTC themes.mozdev.org [Source type: General]
^ There are one or two traders, of course, but we take care to make them behave, and if they don`t we make the place so hot for them they`re glad to go."
[47]
Areas in their path can receive a year's worth of rainfall from a
tropical cyclone passage.
[48]
Human
influence
Image of
Atlanta, Georgia showing temperature
distribution, with blue showing cool temperatures, red warm, and
hot areas appear white.
The fine particulate matter produced by car exhaust and other
human sources of pollution forms
cloud condensation nuclei,
leads to the production of clouds and increases the likelihood of
rain. As commuters and commercial traffic cause pollution to build
up over the course of the week, the likelihood of rain increases:
it peaks by Saturday, after five days of weekday pollution has been
built up. In heavily populated areas that are near the coast, such
as the United States'
Eastern Seaboard,
the effect can be dramatic: there is a 22% higher chance of rain on
Saturdays than on Mondays.
[49] The
urban heat island effect warms cities 0.6 °C (1.1 °F) to 5.6 °C
(10.1 °F) above surrounding suburbs and rural areas. This extra
heat leads to greater upward motion, which can induce additional
shower and thunderstorm activity. Rainfall rates downwind of cities
are increased between 48% and 116%.
.^ Global warming theory 'is falling to bits': '2 recent results published by top scientists cast doubt on the UN IPCC's theory about link between atmospheric CO2 and global warming' .
[50] Some
cities induce a total precipitation increase of 51%.
[51]
Mean surface temperature anomalies during the period 1999 to 2008
with respect to the average temperatures from 1940 to 1980
Increasing temperatures tend to increase evaporation which leads
to more precipitation.
.^ Scientists 'puzzled as to why average global temperatures have stopped rising over the last 10 years' .
^ Update: NOAA removes web page stating 'There is no evidence that CO2 is causing an increase in global temperatures' .
^ NOAA's website: Promotes climate discussion by stating: 'There is no evidence that CO2 is causing an increase in global temperatures' .
Precipitation
generally increased over land north of 30°N from 1900 through 2005
but has declined over the tropics since the 1970s.
.^ Poll: Half of UK public believes there is no proof global warming caused by humans .
^ Equally significant was the time scale, which turned out to be half a millennium or so (in particular, the deep water of the North Atlantic had been down there an average of 650 years).- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Analysis: 3 of 4 measurements show no significant global warming for the last 15 years .
.^ The previous winter had been phenomenally cold and snowy in North America and Europe.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
The Sahel, the Mediterranean, southern Africa and parts of
southern Asia have become drier.
.^ 'Airborne fraction of carbon dioxide has not increased either during the past 150 years or during the most recent 5 decades' .
^ It was just one of a number of studies that led to the recognition, in the 1970s, that there were ocean-atmosphere feedback oscillations on a timescale of a few years to a few decades.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
.^ These studies were no more than suggestive, for the models of the mid 1980s were still extremely limited.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ The upper ocean layers also seemed to mix together more in regions with many storms, and storminess was another thing that might change as the climate changed.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Perhaps, he thought, there had been a transition in the ocean from "a relatively stagnant state" to a state where more rapid mixing brought nutrients to the surface which changed the biochemistry.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
.^ Yet it seemed at least an "intriguing possibility," as they put it, that global warming might shut down the North Atlantic circulation within the next century or so, with grave implications for regional climates.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
^ Monbiot: 'The emails extracted by a hacker from the climatic research unit at the University of East Anglia could scarcely be more damaging' .
^ A few worried that the North Atlantic region was precisely where most of the data on abrupt climate change came from, and where most of the people who thought about it lived.- Ocean Currents and Climate 10 February 2010 13:31 UTC www.aip.org [Source type: FILTERED WITH BAYES]
Hawaii was the only region to show a
decrease (-9.25 percent).
[52]
Patterns
Rainbands spawned near and ahead of
cold fronts can be
squall lines which are able to produce
tornadoes.
[57]
Rainbands associated with cold fronts can be warped by mountain
barriers perpendicular to the front's orientation due to the
formation of a low-level
barrier jet.
[58] Bands
of thunderstorms can form with
sea breeze and
land breeze boundaries,
if enough moisture is present. If sea breeze rainbands become
active enough just ahead of a cold front, they can mask the
location of the cold front itself.
[59]
Banding within the comma head precipitation pattern of an
extratropical cyclone can yield
significant amounts of rain.
[60]
Behind extratropical cyclones, rainbands can form downwind of
relative warm bodies of water such as the
Great Lakes. Downwind of islands, bands of
showers and thunderstorms can develop due to low level wind
convergence downwind of the island edges. Offshore
California, this has been
noted in the wake of cold fronts.
[61]
Rainbands within tropical cyclones are curved in orientation.
Tropical cyclone rainbands contain showers and thunderstorms that,
together with the eyewall and the eye, constitute a
hurricane or
tropical storm. The extent of rainbands around a tropical
cyclone can help determine the cyclone's intensity.
[62]
Measurement
Gages
The standard way of measuring rainfall or snowfall is the
standard rain gauge, which can be found in 100-mm (4-in) plastic
and 200-mm (8-in) metal varieties.
[63] The
inner cylinder is filled by 25 mm (1 in) of rain, with
overflow flowing into the outer cylinder. Plastic gages have
markings on the inner cylinder down to 0.25 mm (0.01 in)
resolution, while metal gauges require use of a stick designed with
the appropriate 0.25 mm (0.01 in) markings. After the
inner cylinder is filled, the amount inside it is discarded, then
filled with the remaining rainfall in the outer cylinder until all
the fluid in the outer cylinder is gone, adding to the overall
total until the outer cylinder is empty.
[64] Other
types of gauges include the popular wedge gauge (the cheapest rain
gauge and most fragile), the tipping bucket rain gauge, and the
weighing rain gauge.
[65] .^ Answer is no : classic use OS X aqua ruler but every other theme I tried based on it got the same bug as "Rain".- mozdev.org - themes: themes/rain 16 January 2010 19:19 UTC themes.mozdev.org [Source type: General]
Any of the above rain gauges can
be made at home, with enough know-how.
[66]
.^ "In weather like this a native hut must be a rather uncomfortable place to live in."
[69]
Remote
sensing
Twenty-four hour rainfall accumulation on the Val d'Irène radar in
Eastern Canada. Zones without data in the east and southwest are
caused by beam blocking from mountains. (Source: Environment
Canada)
One of the main uses of weather radar is to be able to assess
the amount of precipitations fallen over large basins for
hydrological purposes.
[70] For
instance, river flood control, sewer management and dam
construction are all areas where planners use rainfall accumulation
data. Radar-derived rainfall estimates compliment surface station
data which can be used for calibration. To produce radar
accumulations, rain rates over a point are estimated by using the
value of reflectivity data at individual grid points. A radar
equation is then used, which is,
- Z =
ARb,
where Z represents the radar reflectivity, R represents the
rainfall rate, and A and b are constants.
[71]
Satellite derived rainfall estimates use passive
microwave instruments
aboard
polar
orbiting as well as
geostationary weather
satellites to indirectly measure rainfall rates.
[72] .^ For Want of Water: Quenching Las Vegas' Thirst Desert dwellers find summer sizzle, little rainfall Desert oasis drying up Las Vegas weather can be a gamble .- Current Weather Conditions - Las Vegas Sun 17 January 2010 8:29 UTC www.lasvegassun.com [Source type: Reference]
^ The notification box shows up where it should, when it should, but there is no image in it.- mozdev.org - themes: themes/rain 16 January 2010 19:19 UTC themes.mozdev.org [Source type: General]
^ Vermont sets 'all-time record for one snowstorm' .
Intensity
Rainfall intensity is classified according to the rate of
precipitation:
- Light rain — when the precipitation rate is <
2.5 millimetres (0.098 in) per hour
- Moderate rain — when the precipitation rate is between
2.5 millimetres (0.098 in) - 7.6 millimetres
(0.30 in) per hour
- Heavy rain — when the precipitation rate is >
7.6 millimetres (0.30 in) per hour[73]
Return
period
The likelihood or probability of an event with a specified
intensity and duration, is called the
return period or frequency.
[74] The
intensity of a storm can be predicted for any return period and
storm duration, from charts based on historic data for the
location.
[75] .^ National Weather Service records showed that snowfall that sticks around in the valley occurs on average every 20 years.- Current Weather Conditions - Las Vegas Sun 17 January 2010 8:29 UTC www.lasvegassun.com [Source type: Reference]
.^ 'Oceans have a much greater capacity to absorb CO2 than had been previously expected' .
The term
1 in 100 year
storm describes a rainfall event which is extremely rare and
which will occur with a likelihood of only once in a century, so
has a 1 percent likelihood in any given year.
.^ 'Gore can't tell time – thinks most recent Climategate email is more than 10 years old' .
As with all probability events, it is possible to have multiple "1
in 100 Year Storms" in a single year.
[76]
Effect on
agriculture
Rainfall estimates for southern
Japan and the surrounding region from July 20–27,
2009.
Precipitation, especially
rain, has a dramatic effect on
agriculture. All
plants need at least some water to survive,
therefore rain (being the most effective means of watering) is
important to
agriculture. While a regular rain pattern
is usually vital to healthy
plants, too much or too little rainfall can be
harmful, even devastating to
crops.
Drought can kill crops and
increase erosion,
[77] while
overly wet weather can cause harmful
fungus growth.
[78] Plants need varying amounts of
rainfall to survive.
.^ We have three hundred inches in the year.
^ UN climate treaty may need extra year .
^ 'Hundreds of tiny LEDs that light up, depending on the amount of CO2 in the air' .
In areas with wet and dry seasons,
soil nutrients diminish and erosion increases
during the wet season.
[19]
Animals have adaptation and survival strategies for the wetter
regime. The previous dry season leads to food shortages into the
wet season, as the crops have yet to mature.
[80]
Developing countries have noted that their populations show
seasonal weight fluctuations due to food shortages seen before the
first harvest, which occurs late in the wet season.
[81] Rain
may be
harvested through the use of
rainwater tanks
or for non-potable use indoors or for irrigation,
[82] as a
form of
greywater.
Excessive rain during short periods of time can cause flash
floods.
[83]
Culture
Cultural attitudes towards rain differ across the world.
.^ Climate Scare Fading: 'More Americans believe in haunted houses than man-made global warming' - 37% vs. .
^ Warming Establishment Crumbles: More than 140 scientists challenge UN's climate claims in open letter .
^ Climate of Change: Gore speech draws more than 200 protesters in Florida -- 'Boos and chants could be heard' during talk .
[84] Rain
can also bring joy, as some consider it to be soothing or enjoy the
aesthetic appeal of it. In dry places, such as
India,
[85] or
during periods of
drought,
[86] rain
lifts people's moods. In
Botswana, the
Setswana word for rain,
"pula," is used as
the name of the national currency, in
recognition of the economic importance of rain in this desert
country.
[87]
.^ Asian Development Bank warns failure to 'reach climate deal could lead to a collapse of carbon market' .
[88] Many
people find the scent during and immediately after rain pleasant or
distinctive. The source of this scent is
petrichor, an oil produced by plants, then
absorbed by rocks and soil, and later released into the air during
rainfall.
[89]
Forecasting
The Quantitative Precipitation Forecast (abbreviated QPF) is the
expected amount of liquid precipitation accumulated over a
specified time period over a specified area.
[90]
A QPF will be specified when a measurable precipitation type
reaching a minimum threshold is forecast for any hour during a QPF
valid period. Precipitation forecasts tend to be bound by synoptic
hours such as 0000, 0600, 1200 and 1800
GMT. Terrain is considered in QPFs by use
of topography or based upon climatological precipitation patterns
from observations with fine detail.
[91]
Starting in the mid to late 1990s, QPFs were used within hydrologic
forecast models to simulate impact to rivers throughout the United
States.
[92] Forecast models show
significant sensitivity to humidity levels within the
planetary boundary layer, or
in the lowest levels of the atmosphere, which decreases with
height.
[93] QPF
can be generated on a quantitative, forecasting amounts, or a
qualitative, forecasting the probability of a specific amount,
basis.
[94] .^ Peer-Research Determines Gulf of Mexico Medieval Warming Had Higher Temperatures Than Modern Times .
The
forecasts can be verified through use of
rain gage measurements,
weather radar
estimates, or a combination of both. Various skill scores can be
determined to measure the value of the rainfall forecast.
[95]
Role in Köppen
climate classification
Updated Köppen-Geiger climate map
[96]
The Köppen classification depends on average monthly values of
temperature and precipitation. The most commonly used form of the
Köppen classification has five primary types labeled A through E.
Specifically, the primary types are A, tropical; B, dry; C, mild
mid-latitude; D, cold mid-latitude; and E, polar. The five primary
classifications can be further divided into secondary
classifications such as
rain forest,
monsoon,
tropical savanna,
humid subtropical,
humid continental,
oceanic
climate,
Mediterranean climate,
steppe,
subarctic
climate,
tundra,
polar ice cap, and
desert.
Rain forests are characterized by high
rainfall, with definitions
setting minimum normal annual rainfall between
1,750 millimetres (69 in) and 2,000 millimetres
(79 in).
[97] .^ Peer-reviewed study shakes climate debate: '50 years of global cooling predicted' -- Finds CO2 NOT 'major culprit' in temps .
They are widespread on
Africa, and are also found in
India, the northern parts of
South America,
Malaysia, and
Australia.
[98]
The humid subtropical climate zone where winter rainfall (and
sometimes
snowfall) is associated with large
storms that the
westerlies steer from
west to east. Most summer rainfall occurs during
thunderstorms and
from occasional
tropical cyclones.
[99] Humid
subtropical climates lie on the east side continents, roughly
between
latitudes 20° and
40° degrees away from the equator.
[100]
An oceanic (or maritime) climate is typically found along the
west coasts at the middle latitudes of all the world's continents,
bordering cool oceans, as well as southeastern
Australia, and is accompanied by plentiful
precipitation year round.
[101] The
Mediterranean climate regime resembles the climate of the lands in
the
Mediterranean Basin, parts of
western
North
America, parts of
Western and
South
Australia, in southwestern
South Africa and in parts of central
Chile. The climate is characterized
by hot, dry summers and cool, wet winters.
[102] A
steppe is a dry
grassland.
[103]
.^ Chris Mooney: 'The Continuing, Unfortunate Effectiveness of Climate Depot's Morano...a leading nemesis of climate progress...there is, in my mind, little effective counter' .
^ Climate Depot Exclusive - Continuously Updated 'ClimateGate' News Round Up Obama Spokesman Gibbs Blames Record Cold On Global Warming!
[104]
Global
climatology
Approximately 505,000 cubic kilometres
(121,000 cu mi) of water falls as precipitation each year
across the globe with 398,000 cubic kilometres
(95,000 cu mi) of it over the
oceans.
[105]
.^ Plus: 'Global-average sea surface temps in October continued fall from peak in July, despite El Nino conditions' .
.^ Scientists 'puzzled as to why average global temperatures have stopped rising over the last 10 years' .
^ Aussie Scientist: 'More evidence CO2 not culprit -- 'Climate sensitivity associated with CO2 is less than that used in present climate modelling, by a factor of about 3' .
^ 'Gore can't tell time – thinks most recent Climategate email is more than 10 years old' .
[108]
Deserts
The northern half of Africa is primarily
desert or
arid,
containing the
Sahara. Across
Asia, a large annual rainfall minimum, composed primarily of
deserts, stretches from the
Gobi desert in Mongolia
west-southwest through Pakistan and Iran into the
Arabian desert in Saudi Arabia. Most of
Australia is semi-arid or desert,
[109]
making it the world's driest
continent. In South America, the
Andes mountain range blocks
Pacific moisture
that arrives in that continent, resulting in a desertlike climate
just downwind across western Argentina.
[36]
The drier areas of the United States are regions where the
Sonoran desert overspreads the Desert
Southwest, the Great Basin, central Wyoming, and the Willamette
Valley.
[110]
Wetlands
The equatorial region near the
Intertropical Convergence
Zone (ITCZ), or
monsoon trough, is the wettest portion
of the world's continents. Annually, the rain belt within the
tropics marches northward by August, then moves back southward into
the
Southern Hemisphere by February and
March.
[111]
Within Asia, rainfall is favored across its southern portion from
India east and northeast across the Philippines and southern China
into Japan due to the
monsoon advecting moisture primarily from the
Indian Ocean into
the region.
[112] The
monsoon trough can reach as far north as the
40th
parallel in East Asia during August before moving southward
thereafter. Its poleward progression is accelerated by the onset of
the summer monsoon which is characterized by the development of
lower air pressure (a
thermal low) over the warmest part of
Asia.
[113][114][115]
Similar, but weaker, monsoon circulations are present over
North America and
Australia.
[116][117]
.^ New Peer-Reviewed Research: Atlantic Ocean Was 2.7°C Warmer During Roman Warm Period, 2.2°C Warmer During MWP .
[118]
The eastern half of the contiguous United States east of the
98th
meridian, the mountains of the
Pacific Northwest, and the
Sierra
Nevada range are the wetter portions of the nation, with
average rainfall exceeding 30 inches (760 mm) per
year.
[110]
Equatorward of the subtropical ridge,
tropical cyclones enhance
precipitation across southern and eastern sections of the United
States, as well as
Puerto Rico, the
United States Virgin
Islands,
[119] the
Northern Mariana Islands,
[120] Guam, and
American Samoa.
Impact
of the Westerlies
Long-term mean precipitation by month
.^ North Carolina Sea Levels Rising 3mm a year?
^ Amusing: North Carolina sea levels rose at the 'wrong' time .
.^ 'On average each day in 1855 more than 50 tons of horse excrement was removed from only one street' .
During the fall, winter, and
spring, Pacific
storm systems bring most of
Hawaii and the western United States much of
their precipitation.
[118]
Over the top of the ridge, the jet stream brings a summer
precipitation maximum to the
Great Lakes.
.^ Rush Limbaugh Praises Climate Depot: 'It's a great place to keep up on the global warming debate' .
[121]
The
El Niño-Southern
Oscillation affects the precipitation distribution, by altering
rainfall patterns across the western United States,
[122]
Midwest,
[123][124] the
Southeast,
[125] and
throughout the tropics.
.^ 'Global warming leads to too many polar bears' .
^ Chinese debate positive side of global warming: 'Dynasties were more prosperous' when weather was warm' .
^ More Data Questions: 'There is at least one temp station where trend has been artificially increased to give a false warming where raw data shows cooling' .
Wettest
known locations
.^ 'A hypocrite as well as a liar': IPCC's Pachauri resides in 'one of the most expensive places to live in India' .
.^ National Weather Service records showed that snowfall that sticks around in the valley occurs on average every 20 years.- Current Weather Conditions - Las Vegas Sun 17 January 2010 8:29 UTC www.lasvegassun.com [Source type: Reference]
[126] .^ After many years of married life he had learned that it was more conducive to peace to leave his wife with the last word.
^ Developing countries now emit more 'greenhouse gas' than rich countries .
^ Climate of Change: Gore speech draws more than 200 protesters in Florida -- 'Boos and chants could be heard' during talk .
It has
been promoted in tourist literature for many years as the wettest
spot in the world.
[128] Lloró, a town situated in
Chocó,
Colombia, is probably the
place with the largest measured rainfall in the world, averaging
13,300 mm per year (523.6 in).
[129] The
Department of Chocó is extraordinarily humid. Tutunendo, a small
town situated in the same department, is one of the wettest places
on earth, averaging 11,394 mm per year (448 in); in 1974 the
town received 26,303 mm (86 ft 3½ in), the largest annual
rainfall measured in Colombia. Unlike Cherrapunji, which receives
most of its rainfall between April and September, Tutunendo
receives rain almost uniformly distributed throughout the year.
[130] .^ 'Takes between 100 to 1,000 years for a golf ball to decompose naturally' -- '300 million balls are lost or discarded in U.S. alone' .
Storms in
Chocó can drop 500 mm (19.7 in) of rainfall in a day.
.^ After many years of married life he had learned that it was more conducive to peace to leave his wife with the last word.
^ 'Gore can't tell time – thinks most recent Climategate email is more than 10 years old' .
^ Scientist: 'For more than 90% of recent geological time Earth has been colder than today' .
Outside of
Earth
On
Titan,
Saturn's largest moon, infrequent
methane rain is thought to
carve the moon's numerous surface channels.
[131
] On
Venus,
sulfuric acid virga evaporates 25 km from
the surface. There is likely to be rain of various compositions in
the upper atmospheres of the
gas giants, as well as precipitation of
liquid
neon and
helium in the deep atmospheres.
See also
References
- ^
Steve Kempler (2009). "Parameter information
page". NASA Goddard Space Flight
Center. http://daac.gsfc.nasa.gov/PIP/shtml/atmospheric_water_vapor_or_humidity.shtml. Retrieved
2008-12-27.
- ^
Naval Meteorology and Oceanography
Command (2007). "Atmospheric Moisture".
United
States Navy. http://www.navmetoccom.navy.mil/pao/Educate/WeatherTalk2/indexatmosp.htm. Retrieved
2008-12-27.
- ^
FMI (2007). "Fog And Stratus -
Meteorological Physical Background". Zentralanstalt für
Meteorologie und Geodynamik. http://www.zamg.ac.at/docu/Manual/SatManu/main.htm?/docu/Manual/SatManu/CMs/FgStr/backgr.htm. Retrieved
2009-02-07.
- ^
Glossary of Meteorology (2009). "Adiabatic Process". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?id=adiabatic-process1. Retrieved
2008-12-27.
- ^
TE Technology, Inc (2009). "Peltier Cold Plate". http://www.tetech.com/Cold-Plate-Coolers.html. Retrieved
2008-12-27.
- ^
Glossary of Meteorology (2009). "Radiational cooling". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?p=1&query=radiational+cooling&submit=Search. Retrieved
2008-12-27.
- ^
Robert Fovell (2004). "Approaches to
saturation". University of California in Los
Angelese. http://www.atmos.ucla.edu/~fovell/AS3downloads/saturation.pdf. Retrieved
2009-02-07.
- ^ Robert Penrose Pearce (2002). Meteorology at the
Millennium. Academic Press. p. 66. ISBN
978-0-12-548035-2. http://books.google.com/books?id=QECy_UBdyrcC&pg=PA66&lpg=PA66&dq=ways+to+moisten+the+atmosphere&source=web&ots=-0MYq5qyS6&sig=gz5lOAPIc54v5qfO7nZ098KmVGE&hl=en&sa=X&oi=book_result&resnum=6&ct=result. Retrieved
2009-01-02.
- ^
National Weather Service
Office, Spokane, Washington (2009). "Virga and Dry
Thunderstorms". http://www.wrh.noaa.gov/otx/outreach/ttalk/virga.php. Retrieved
2009-01-02.
- ^
Bart van den Hurk and Eleanor Blyth
(2008). "Global maps of Local
Land-Atmosphere coupling". KNMI. http://www.knmi.nl/~hurkvd/Loco_workshop/Workshop_report.pdf. Retrieved
2009-01-02.
- ^
Krishna Ramanujan and Brad Bohlander
(2002). "Landcover changes may rival
greenhouse gases as cause of climate change". National Aeronautics and Space
Administration Goddard Space Flight
Center. http://www.gsfc.nasa.gov/topstory/20020926landcover.html. Retrieved
2009-01-02.
- ^
National Weather Service
JetStream (2008). "Air Masses". http://www.srh.weather.gov/srh/jetstream/synoptic/airmass.htm. Retrieved
2009-01-02.
- ^ a
b
Dr. Michael Pidwirny (2008). "CHAPTER 8: Introduction to
the Hydrosphere (e). Cloud Formation Processes". Physical
Geography. http://www.physicalgeography.net/fundamentals/8e.html. Retrieved
2009-01-01.
- ^
Glossary of Meteorology (June 2000). "Warm Rain Process". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?id=warm-rain-process1. Retrieved
2010-01-15.
- ^
Paul Sirvatka (2003). "Cloud Physics:
Collision/Coalescence; The Bergeron Process". College of
DuPage. http://weather.cod.edu/sirvatka/bergeron.html. Retrieved
2009-01-01.
- ^
Alistair B. Fraser (2003-01-15). "Bad Meteorology: Raindrops
are shaped like teardrops.". Pennsylvania State
University. http://www.ems.psu.edu/~fraser/Bad/BadRain.html. Retrieved
2008-04-07.
- ^
United States Geological
Survey (2009). "Are raindrops tear
shaped?". United States
Department of the Interior. http://ga.water.usgs.gov/edu/raindropshape.html. Retrieved
2008-12-27.
- ^
Paul Rincon (2004-07-16). "Monster raindrops delight
experts". British Broadcasting
Company. http://news.bbc.co.uk/2/hi/science/nature/3898305.stm. Retrieved
2009-11-30.
- ^ a
b
c
J . S. 0guntoyinbo and F. 0. Akintola
(1983). "Rainstorm characteristics
affecting water availability for agriculture". IAHS Publication
Number 140. http://www.cig.ensmp.fr/~iahs/redbooks/a140/iahs_140_0063.pdf. Retrieved
2008-12-27.
- ^
Robert A. Houze Jr (October 1997).
"Stratiform Precipitation in
Regions of Convection: A Meteorological Paradox?". Bulletin
of the American Meteorological
Society 78 (10): 2179–2196. http://ams.allenpress.com/archive/1520-0477/78/10/pdf/i1520-0477-78-10-2179.pdf. Retrieved
2008-12-27.
- ^
Norman W. Junker (2008). "An ingredients based
methodology for forecasting precipitation associated with
MCS’s". Hydrometeorological
Prediction Center. http://www.hpc.ncep.noaa.gov/research/mcs_web_test_test_files/Page882.htm. Retrieved
2009-02-07.
- ^
"Falling raindrops hit 5 to 20
mph speeds". Weather Quest. http://www.wonderquest.com/falling-raindrops.htm. Retrieved
2008-04-08.
- ^ Alaska Air Flight Service Station
(2007-04-10). "SA-METAR". Federal Aviation
Administration. http://www.alaska.faa.gov/fai/afss/metar%20taf/sametara.htm. Retrieved
2009-08-29.
- ^
G. E. Likens, W. C. Keene, J. M.
Miller and J. N. Galloway (1987). "Chemistry of precipitation from
a remote, terrestrial site in Australia". Journal of
Geophysical Research 92 (13):
299-314.
- ^
Joel S. Levine, Tommy R. Augustsson,
Iris C. Andersont, James M. Hoell Jr., and Dana A. Brewer (1984).
"Tropospheric sources of NOx:
Lightning and biology". Atmospheric Environment
18 (9): 1797–1804. doi:10.1016/0004-6981(84)90355-X. PMID 11540827. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B757C-488FRK0-2N&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&_docanchor=&view=c&_searchStrId=1001036955&_rerunOrigin=google&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=05e7b4ab4444bada8188d84c8a19ccc0. Retrieved
2009-09-04.
- ^
Glossary of Meteorology (June 2000). "Acid Rain". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?p=1&query=acid+rain&submit=Search. Retrieved
2010-01-15.
- ^
Eli Kintisch (January 2008). "23. Acid Rain Intensifies
Threat To Marine Life". Discover. http://discovermagazine.com/2008/jan/acid-rain-intensifies-threat-to-marine-life. Retrieved
2010-01-15.
- ^ a
b
B. Geerts (2002). "Convective and stratiform
rainfall in the tropics". University of Wyoming. http://www-das.uwyo.edu/~geerts/cwx/notes/chap10/con_str.html. Retrieved
2007-11-27.
- ^ David Roth (2006). "Unified Surface Analysis
Manual". Hydrometeorological
Prediction Center. http://www.hpc.ncep.noaa.gov/sfc/UASfcManualVersion1.pdf. Retrieved
2006-10-22.
- ^
Robert Houze (October 1997). "Stratiform Precipitation in
Regions of Convection: A Meteorological Paradox?". Bulletin
of the American Meteorological Society 78
(10): 2179. doi:10.1175/1520-0477(1997)078<2179:SPIROC>2.0.CO;2. http://ams.allenpress.com/archive/1520-0477/78/10/pdf/i1520-0477-78-10-2179.pdf. Retrieved
2007-11-27.
- ^
Glossary of Meteorology (2009). "Graupel". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?p=1&query=graupel&submit=Search. Retrieved
2009-01-02.
- ^
Toby N. Carlson (1991). Mid-latitude Weather
Systems. Routledge. p. 216. ISBN
978-0-04-551115-0. http://books.google.com/books?id=2lIVAAAAIAAJ&pg=PA216&lpg=PA216&dq=where+convection+occurs+in+the+mid-latitudes&source=bl&ots=zS1wy_LX-l&sig=hs-dTbXpXIvyonGeakw2kgqkFNk&hl=en&ei=SJ6NSf74EZ6DtweHxdGDCw&sa=X&oi=book_result&resnum=5&ct=result. Retrieved
2009-02-07.
- ^
Diana Leone (2002). "Rain supreme". Honolulu
Star-Bulletin. http://starbulletin.com/2002/05/27/news/story3.html. Retrieved
2008-03-19.
- ^ Steven Businger and
Thomas Birchard, Jr. A Bow Echo and Severe Weather
Associated with a Kona Low in Hawaii. Retrieved on
2007-05-22.
- ^
Western Regional Climate Center (2002).
"Climate of Hawaii". http://www.wrcc.dri.edu/narratives/HAWAII.htm. Retrieved
2008-03-19.
- ^ a
b
Paul E. Lydolph (1985). The Climate of the
Earth. Rowman & Littlefield. p. 333. ISBN
978-0-86598-119-5. http://books.google.com/books?id=bBjIuXHEgZ4C&pg=PA333&lpg=PA333&dq=effect+of+Andes+on+rainfall+in+Chile&source=web&ots=HwFkS0f4BQ&sig=ibCwQhN-vZPpAWylwrWOgaRlfTo&hl=en&sa=X&oi=book_result&resnum=9&ct=result. Retrieved
2009-01-02.
- ^
Michael A. Mares (1999). Encyclopedia of
Deserts. University of Oklahoma Press.
p. 252. ISBN
978-0-8061-3146-7. http://books.google.com/books?id=g3CbqZtaF4oC&pg=PA252&lpg=PA252&dq=sierra+nevada+leads+to+great+basin+desert&source=bl&ots=uWzrnwnUPA&sig=0gl6AdoVQDlRPnAOphPG5txHd3Q&hl=en&sa=X&oi=book_result&resnum=3&ct=result. Retrieved
2009-01-02.
- ^
Adam Ganson (2003). "Geology of Death Valley".
Indiana
University. http://www.indiana.edu/~sierra/papers/2003/Ganson.html. Retrieved
2009-02-07.
- ^
Glossary of Meteorology (2009). "Rainy season". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?id=rainy-season1. Retrieved
2008-12-27.
- ^
Costa Rica Guide (2005). "When to Travel to Costa Rica".
ToucanGuides. http://costa-rica-guide.com/when.htm. Retrieved
2008-12-27.
- ^
Michael Pidwirny (2008). "CHAPTER 9: Introduction to
the Biosphere". PhysicalGeography.net.
http://www.physicalgeography.net/fundamentals/9k.html. Retrieved
2008-12-27.
- ^ Elisabeth M. Benders-Hyde (2003). "World Climates". Blue
Planet Biomes. http://www.blueplanetbiomes.org/climate.htm. Retrieved
2008-12-27.
- ^
Mei Zheng (2000). "The sources and
characteristics of atmospheric particulates during the wet and dry
seasons in Hong Kong". University of Rhode
Island. http://digitalcommons.uri.edu/dissertations/AAI9989458/. Retrieved
2008-12-27.
- ^
S. I. Efe, F. E. Ogban, M. J.
Horsfall, E. E. Akporhonor (2005). "Seasonal Variations of
Physico-chemical Characteristics in Water Resources Quality in
Western Niger Delta Region, Nigeria". Journal of Applied
Scientific Environmental Management 9 (1):
191–195. ISSN 1119-8362. https://tspace.library.utoronto.ca/bitstream/1807/6445/1/ja05036.pdf. Retrieved
2008-12-27.
- ^
C. D. Haynes, M. G. Ridpath, M. A. J.
Williams (1991). Monsoonal
Australia. Taylor & Francis. p. 90. ISBN
978-90-6191-638-3. http://books.google.com/books?id=ZhvtSmJYuN4C&pg=PA91&lpg=PA91&dq=wet+season+characteristics&source=web&ots=RgIkJ2tZp3&sig=nCLkFclils6CqFgiUoSs7RhBsXU&hl=en&sa=X&oi=book_result&resnum=4&ct=result#PPA90,M1. Retrieved
2008-12-27.
- ^
Chris Landsea (2007).
"Subject: D3) Why do tropical
cyclones' winds rotate counter-clockwise (clockwise) in the
Northern (Southern) Hemisphere?". National Hurricane
Center. http://www.aoml.noaa.gov/hrd/tcfaq/D3.html. Retrieved
2009-01-02.
- ^ Climate Prediction Center
(2005). "2005 Tropical Eastern North
Pacific Hurricane Outlook". National
Oceanic and Atmospheric Administration.
http://www.cpc.ncep.noaa.gov/products/Epac_hurr/Epac_hurricane.html. Retrieved
2006-05-02.
- ^
Jack Williams (2005). "Background: California's
tropical storms". USA
Today. http://www.usatoday.com/weather/whhcalif.htm. Retrieved
2009-02-07.
- ^
R. S. Cerveny and R. C. Balling
(1998-08-06). "Weekly cycles of air pollutants, precipitation and
tropical cyclones in the coastal NW Atlantic region".
Nature 394: 561-563. doi:10.1038/29043.
- ^
Dale Fuchs (2005-06-28). "Spain goes hi-tech to beat
drought". The
Guardian. http://www.guardian.co.uk/weather/Story/0,2763,1516375,00.html. Retrieved
2007-08-02.
- ^
Goddard Space Flight Center
(2002-06-18). "NASA Satellite Confirms Urban Heat Islands
Increase Rainfall Around Cities". National Aeronautics and Space
Administration. http://www.gsfc.nasa.gov/topstory/20020613urbanrain.html. Retrieved
2009-07-17.
- ^
Climate Change Division (2008-12-17). "Precipitation and Storm
Changes". Environment Protection Agency. http://www.epa.gov/climatechange/science/recentpsc.html. Retrieved
2009-07-17.
- ^
Glossary of Meteorology (2009). Rainband. Retrieved on
2008-12-24.
- ^
Glossary of Meteorology (2009). Banded structure.
Retrieved on 2008-12-24.
- ^
Owen Hertzman (1988). Three-Dimensional Kinematics
of Rainbands in Midlatitude Cyclones. Retrieved on
2008-12-24
- ^
Yuh-Lang Lin (2007). Mesoscale Dynamics.
Retrieved on 2008-12-25.
- ^
Glossary of Meteorology (2009). Prefrontal squall line.
Retrieved on 2008-12-24.
- ^
J. D. Doyle (1997). The influence of mesoscale
orography on a coastal jet and rainband. Retrieved on
2008-12-25.
- ^
A. Rodin (1995). Interaction of a cold front
with a sea-breeze front numerical simulations. Retrieved on
2008-12-25.
- ^
David R. Novak, Lance F. Bosart, Daniel Keyser, and Jeff S.
Waldstreicher (2002). A CLIMATOLOGICAL AND
COMPOSITE STUDY OF COLD SEASON BANDED PRECIPITATION IN THE
NORTHEAST UNITED STATES. Retrieved on 2008-12-26.
- ^
Ivory J. Small (1999). AN OBSERVATIONAL STUDY OF
ISLAND EFFECT BANDS: PRECIPITATION PRODUCERS IN SOUTHERN
CALIFORNIA. Retrieved on 2008-12-26.
- ^ University of
Wisconsin–Madison (1998).Objective Dvorak
Technique. Retrieved on 2006-05-29.
- ^
National Weather Service
Office, Northern Indiana (2009). "8 Inch Non-Recording Standard
Rain Gauge". http://www.crh.noaa.gov/iwx/program_areas/coop/8inch.php. Retrieved
2009-01-02.
- ^
Chris Lehmann (2009). "10/00". Central
Analytical Laboratory. http://nadp.sws.uiuc.edu/CAL/2000_reminders-4thQ.htm. Retrieved
2009-01-02.
- ^
National Weather Service
(2009). "Glossary: W". http://www.weather.gov/glossary/index.php?letter=w. Retrieved
2009-01-01.
- ^
Discovery School (2009). "Build Your Own Weather
Station". Discovery Education. http://school.discovery.com/lessonplans/activities/weatherstation/itsrainingitspouring.html. Retrieved
2009-01-02.
- ^
"Community Collaborative Rain,
Hail & Snow Network Main Page". Colorado Climate Center.
2009. http://cocorahs.org. Retrieved
2009-01-02.
- ^
The Globe Program (2009). "Global Learning and
Observations to Benefit the Environment Program". http://www.globe.gov/fsl/welcome/welcomeobject.pl. Retrieved
2009-01-02.
- ^
National Weather Service
(2009). "NOAA's National Weather Service Main Page". http://www.nws.noaa.gov. Retrieved
2009-01-01.
- ^
Kang-Tsung Chang, Jr-Chuan Huang,
Shuh-Ji Kao, and Shou-Hao Chiang (2009). "Radar Rainfall Estimates for
Hydrologic and Landslide Modeling". Data Assimilation for
Atmospheric, Oceanic and Hydrologic Applications: 127-145. doi:10.1007/978-3-540-71056-1_6. ISBN
978-3-540-71056-1. http://www.springerlink.com/content/g5447473427jl6w1/. Retrieved
2010-01-15.
- ^
Eric Chay Ware (August 2005). "Corrections to
Radar-Estimated Precipitation Using Observed Rain Gauge Data: A
Thesis". Cornell University. p. 1. http://ecommons.library.cornell.edu/bitstream/1813/2115/1/pdfthesis.pdf. Retrieved
2010-01-02.
- ^
Pearl Mngadi, Petrus JM Visser, and
Elizabeth Ebert (October 2006). "Southern Africa Satellite
Derived Rainfall Estimates Validation". International
Precipitation Working Group. p. 1. http://www.isac.cnr.it/~ipwg/meetings/melbourne/papers/Mngadi.pdf. Retrieved
2010-01-05.
- ^
Glossary of Meteorology (June 2000). "Rain". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?id=rain1. Retrieved
2010-01-15.
- ^
Glossary of Meteorology (2009). "Return period". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?id=return-period1. Retrieved
2009-01-02.
- ^
Glossary of Meteorology (2009). "Rainfall intensity return
period". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?p=1&query=return+period&submit=Search. Retrieved
2009-01-02.
- ^
Boulder Area Sustainability Information
Network (2005). "What is a 100 year
flood?". Boulder Community Network. http://bcn.boulder.co.us/basin/watershed/flood.html. Retrieved
2009-01-02.
- ^
Bureau of
Meteorology (2010). "Living With Drought".
Commonwealth of Australia. http://www.bom.gov.au/climate/drought/livedrought.shtml. Retrieved
2010-01-15.
- ^
Robert Burns (2007-06-06). "Texas Crop and Weather".
Texas A&M University. http://agnewsarchive.tamu.edu/dailynews/stories/CROP/Jun0607a.htm. Retrieved
2010-01-15.
- ^
James D. Mauseth (2006-07-07). "Mauseth Research: Cacti".
University of Texas. http://www.sbs.utexas.edu/mauseth/researchoncacti/. Retrieved
2010-01-15.
- ^
A.
Roberto Frisancho (1993). Human Adaptation and
Accommodation. University of Michigan Press, pp. 388. ISBN
9780472095117. Retrieved on 2008-12-27.
- ^
Marti J. Van Liere, Eric-Alain D.
Ategbo, Jan Hoorweg, Adel P. Den Hartog, and Joseph G. A. J.
Hautvast (1994). "The significance of
socio-economic characteristics for adult seasonal body-weight
fluctuations: a study in north-western Benin". British
Journal of Nutrition (Cambridge University Press)
72: 479–488. http://journals.cambridge.org/download.php?file=%2FBJN%2FBJN72_03%2FS0007114594000504a.pdf&code=40a3bcb87f8abc243d961c531b3262e2.
- ^
Texas Department of Environmental
Quality (2008-01-16). "Harvesting, Storing, and
Treating Rainwater for Domestic Indoor Use". Texas A&M University. http://rainwaterharvesting.tamu.edu/drinking/gi-366_2021994.pdf. Retrieved
2010-01-15.
- ^
Glossary of Meteorology (June 2000). "Flash Flood". American Meteorological
Society. http://amsglossary.allenpress.com/glossary/search?p=1&query=flash+flood&submit=Search. Retrieved
2010-01-15.
- ^
A. G. Barnston (1986-12-10). "The effect of weather on
mood, productivity, and frequency of emotional crisis in a
temperate continental climate". International Journal of
Biometeorology 32 (4): 134-143. doi:10.1007/BF01044907. http://www.springerlink.com/content/j6687l0q639541p3/. Retrieved
2010-01-15.
- ^
IANS (2009-03-23). "Sudden spell of rain lifts
mood in Delhi". Thaindian news. http://www.thaindian.com/newsportal/enviornment/sudden-spell-of-rain-lifts-mood-in-delhi_100172192.html. Retrieved
2010-01-15.
- ^
William Pack (2009-09-11). "Rain lifts moods of
farmers". San Antonio Express-News. http://www.mysanantonio.com/business/Rain_lifts_mood_of_farmers.html. Retrieved
2010-01-15.
- ^
Robyn Cox (2007). "Glossary of Setswana and
Other Words". http://www.pulapulapula.co.uk/Glossary.html. Retrieved
2010-01-15.
- ^
Allen Burton and Robert Pitt (2002).
CRC Press, LLC. p. 4. http://unix.eng.ua.edu/~rpitt/Publications/BooksandReports/Stormwater%20Effects%20Handbook%20by%20%20Burton%20and%20Pitt%20book/chp1.pdf. Retrieved
2010-01-15.
- ^ Bear, I.J.; R.G. Thomas (March 1964).
"Nature of argillaceous odour". Nature
201 (4923): 993–995. doi:10.1038/201993a0.
- ^ Jack S. Bushong (1999). "Quantitative Precipitation
Forecast: Its Generation and Verification at the Southeast River
Forecast Center". University of Georgia. http://cms.ce.gatech.edu/gwri/uploads/proceedings/1999/BushongJ-99.pdf. Retrieved
2008-12-31.
- ^
Daniel Weygand (2008). "Optimizing Output From QPF
Helper". National Weather Service
Western Region. http://www.wrh.noaa.gov/wrh/talite0821.pdf. Retrieved
2008-12-31.
- ^
Noreen O. Schwein (2009). "Optimization of quantitative
precipitation forecast time horizons used in river forecasts".
American Meteorological
Society. http://ams.confex.com/ams/89annual/techprogram/paper_149707.htm. Retrieved
2008-12-31.
- ^
Christian Keil, Andreas Röpnack,
George C. Craig, and Ulrich Schumann (2008-12-31). "Sensitivity of quantitative
precipitation forecast to height dependent changes in
humidity". Geophysical Research Letters
35. http://www.agu.org/pubs/crossref/2008/2008GL033657.shtml.
- ^
P. Reggiani and A. H. Weerts
(February 2008). "Probabilistic Quantitative
Precipitation Forecast for Flood Prediction: An Application".
Journal of Hydrometeorology 9 (1):
76–95. http://ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F2007JHM858.1&ct=1. Retrieved
2008-12-31.
- ^ Charles Lin (2005). "Quantitative Precipitation
Forecast (QPF) from Weather Prediction Models and Radar Nowcasts,
and Atmospheric Hydrological Modelling for Flood Simulation".
Achieving Technological Innovation in Flood Forecasting
Project. http://www.actif-ec.net/Workshop2/Presentations/ACTIF_P_S1_02.pdf. Retrieved
2009-01-01.
- ^
Peel, M. C. and Finlayson, B. L. and
McMahon, T. A. (2007). "Updated world map of the
Köppen-Geiger climate classification". Hydrol. Earth Syst.
Sci. 11: 1633–1644. ISSN 1027-5606. http://www.hydrol-earth-syst-sci.net/11/1633/2007/hess-11-1633-2007.html.
(direct: Final Revised
Paper)
- ^
Susan Woodward (1997-10-29). "Tropical Broadleaf Evergreen
Forest: The Rainforest". Radford University. http://www.radford.edu/~swoodwar/CLASSES/GEOG235/biomes/rainforest/rainfrst.html. Retrieved
2008-03-14.
- ^ Susan Woodward (2005-02-02). "Tropical Savannas". Radford
University. http://www.radford.edu/~swoodwar/CLASSES/GEOG235/biomes/savanna/savanna.html. Retrieved
2008-03-16.
- ^
"Humid subtropical
climate". Encyclopædia Britannica.
Encyclopædia Britannica Online. 2008. http://www.britannica.com/eb/article-53358/climate. Retrieved
2008-05-14.
- ^
Michael Ritter (2008-12-24). "Humid Subtropical
Climate". University of
Wisconsin–Stevens Point. http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/climate_systems/humid_subtropical.html. Retrieved
2008-03-16.
- ^ Lauren Springer Ogden (2008).
Plant-Driven Design. Timber Press. p. 78. ISBN
9780881928778.
- ^ Michael Ritter (2008-12-24). "Mediterranean or Dry Summer
Subtropical Climate". University of
Wisconsin–Stevens Point. http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/climate_systems/mediterranean.html. Retrieved
2009-07-17.
- ^ Brynn Schaffner and Kenneth Robinson
(2003-06-06). "Steppe Climate". West
Tisbury Elementary School. http://www.blueplanetbiomes.org/steppe_climate_page.htm. Retrieved
2008-04-15.
- ^ Michael Ritter (2008-12-24). "Subarctic Climate". University of
Wisconsin–Stevens Point. http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/climate_systems/subarctic.html. Retrieved
2008-04-16.
- ^ Dr. Chowdhury's Guide to Planet Earth (2005).
"The Water Cycle".
WestEd. http://www.planetguide.net/book/chapter_2/water_cycle.html. Retrieved
2006-10-24.
- ^ Publications Service Center (2001-12-18). "What is a desert?". United
States Geologic Survey. http://pubs.usgs.gov/gip/deserts/what/. Retrieved
2010-01-15.
- ^ According to What is a desert?, the 250 mm threshold
definition is attributed to Peveril Meigs.
- ^ "desert". Encyclopædia
Britannica online. http://www.britannica.com/eb/article-70815/desert. Retrieved
2008-02-09.
- ^ "About Biodiversity".
Department of the Environment and Heritage. Archived from the original on
2007-02-05. http://web.archive.org/web/20070205015628/www.environment.gov.au/biodiversity/about-biodiversity.html. Retrieved
2007-09-18.
- ^ a
b
NationalAtlas.gov (2009-09-17). "Precipitation of the
Individual States and of the Conterminous States". United States
Department of the Interior. http://www.nationalatlas.gov/printable/precipitation.html. Retrieved
2010-01-15.
- ^ Todd
Mitchell (October 2001). "Africa Rainfall
Climatology". University of Washington. http://jisao.washington.edu/data/ud/africa/. Retrieved
2010-01-02.
- ^ W. Timothy Liu, Xiaosu Xie, and Wenqing
Tang (2006). "Monsoon, Orography, and
Human Influence on Asian Rainfall". Proceedings of the
First International Symposium in Cloud-prone & Rainy Areas
Remote Sensing (CARRS), Chinese University of Hong Kong
(National Aeronautic and Space
Administration Jet Propulsion
Laboratory). http://airsea-www.jpl.nasa.gov/publication/paper/CARRS-ms5.pdf. Retrieved
2010-01-04.
- ^ National Centre for Medium Range Forecasting
(2004-10-23). "Chapter-II Monsoon-2004:
Onset, Advancement and Circulation Features". India Ministry of
Earth Sciences. http://www.ncmrwf.gov.in/Chapter-II.pdf. Retrieved
2008-05-03.
- ^ Australian Broadcasting
Corporation (1999-08-11). "Monsoon". http://www.abc.net.au/storm/monsoon/print.htm. Retrieved
2008-05-03.
- ^ Dr. Alex DeCaria. Lesson 4 – Seasonal-mean Wind
Fields. Retrieved on 2008-05-03.
- ^ David J. Gochis, Luis Brito-Castillo, and
W. James Shuttleworth (2006-01-10). "Hydroclimatology of the
North American Monsoon region in northwest Mexico". Journal
of Hydrology 316: 53-70. doi:10.1016/j.jhydrol.2005.04.021. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V6C-4GX0CS2-1&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&_docanchor=&view=c&_searchStrId=1155477058&_rerunOrigin=google&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=39b2d61a04776e3b1b2b56071cdb5b2a. Retrieved
2010-01-05.
- ^ Bureau of Meteorology. Climate of Giles.
Retrieved on 2008-05-03.
- ^ a
b
J. Horel. Normal Monthly Precipitation,
Inches. Retrieved on 2008-03-19.
- ^ Central Intelligence
Agency. The World Factbook -- Virgin
Islands. Retrieved on 2008-03-19.
- ^ BBC. Weather Centre - World
Weather - Country Guides - Northern Mariana Islands. Retrieved
on 2008-03-19.
- ^ Walker S. Ashley,
Thomas L. Mote, P. Grady Dixon, Sharon L. Trotter, Emily J. Powell,
Joshua D. Durkee, and Andrew J. Grundstein. Distribution of Mesoscale
Convective Complex Rainfall in the United States. Retrieved on
2008-03-02.
- ^ John Monteverdi and Jan Null.
Western Region Technical
Attachment NO. 97-37 November 21, 1997: El Niño and California
Precipitation. Retrieved on 2008-02-28.
- ^ Southeast Climate Consortium.
SECC Winter Climate
Outlook. Retrieved on 2008-02-29.
- ^ Reuters (2007-02-16). "La Nina could mean dry
summer in Midwest and Plains". http://www.reuters.com/article/domesticNews/idUSN1619766420070216. Retrieved
2008-02-29.
- ^ Climate Prediction Center. El Niño (ENSO) Related
Rainfall Patterns Over the Tropical Pacific. Retrieved on
2008-02-28.
- ^ A.
J. Philip (2004-10-12). "Mawsynram in India". Tribune News Service. http://www.clas.ufl.edu/users/jsouthwo/web/6-per-page-Wettest-Mawsynram-in-India.pdf. Retrieved
2010-01-05.
- ^ Bureau of Meteorology (2010). "Significant Weather -
DECEMBER 2000 (Rainfall)". Commonwealth of Australia. http://www.bom.gov.au/inside/services_policy/public/sigwxsum/sigw1200.shtml#rain. Retrieved
2010-01-15.
- ^ "USGS 220427159300201 1047.0
Mt. Waialeale Rain Gage nr Lihue, Kauai, HI". USGS Real-time
rainfall data at Waiʻaleʻale
Raingauge. http://waterdata.usgs.gov/hi/nwis/uv?site_no=220427159300201&PARAmeter_cd=00045. Retrieved
2008-12-11.
- ^ National Climatic Data
Center (2005-08-09). "Global Measured Extremes of
Temperature and Precipitation". National
Oceanic and Atmospheric Administration.
http://www.ncdc.noaa.gov/oa/climate/globalextremes.html. Retrieved
2007-01-18.
- ^ Alfred Rodríguez Picódate (2008-02-07). "Tutunendaó, Choco: la ciudad
colombiana es muy lluviosa". El Periódico.com. http://www.elperiodico.com/default.asp?idpublicacio_PK=46&idioma=CAS&idnoticia_PK=523370&idseccio_PK=1038. Retrieved
2008-12-11.
- ^
Emily Lakdawalla (January 21, 2004). "Titan: Arizona in an
Icebox?". The Planetary Society. http://www.planetary.org/news/2005/huygens_science-results_0121.html. Retrieved
2005-03-28.
External
links