It seems clear to me that the sentence is about responses to a shift from one climate regime, the recent past and present day, to another,
with less precipitation, in the future (it is the IPCC climate change impacts report after all, and they do say `... not necessarily producing gradual changes between the current and the future situation»).
As water quantities slow
with less precipitation, a concentration of nutrients and sediments reduces the water quality.
The chart's green curve indicates that those periods
with less precipitation (i.e. droughts) are more common when cooler temps prevail - more arid conditions, with less food production make people (and societies) rather restless.
For example, in Southern California, tropical widening may be associated
with less precipitation.
Not exact matches
The term, coined in the mid-19th century, typically refers to
precipitation with a pH of
less than 5.2.
«Much
less is known about the impacts of freshwater influx from the
precipitation associated
with a hurricane.»
They are more likely to fail in dryer regions
with less frequent and predictable
precipitation, such as the Great Plains, where environmental conditions limit production of bioenergy grasses.
Based on these figures, I suppose that the West Greenland ice melting was larger in the 1930 - 1950 period than in the 1985 - 2005 period... Alternative explanations may be that the Greenland ice melting has nothing to do
with temperature, but
with more insolation (
less clouds),
less precipitation, more soot deposit,...
If it reaches this height, it's
less likely to be brought back down to earth in
precipitation or mixed
with other particles, extending its presence in the atmosphere from about a week to about a year.
Many areas don't see enough winter
precipitation to justify the cost of an extra set of tires, so vehicle manufacturers stick
with less focused equipment, tires that are useful in most regions for most of the year, in order to keep prices down.
Summers tend to be dry
with less than one - third that of the wettest winter month, and
with less than 30 mm (1.18 in) of
precipitation in a summer month.
Ponta Delgada has a borderline humid subtropical (Cfa) and Mediterranean climate (Csa) under the Köppen classification
with strong oceanic (Cfb) influence, due to high levels of
precipitation throughout the year combined
with less sunshine, and because only one warm month just reaches 22.1 °C (71.8 °F).
A model by the Purdue Climate Change Research Center in West Lafayette forecasts, by 2050, the full growing seasons will expand by one month; there will be 33 to 45 more days
with temperatures above 90 degrees; an increase in
precipitation between 14 percent and 22 percent; and 24 days to 36 days
less snow cover.
In that case (along
with greater
precipitation, and the
precipitation belt moving to higher latitudes), there could be more snow in the winter & greater melting in the summer (in higher latitudes), while I'd think the lower latitudes (
with less precip) and the local mean temp being higher, would melt the glaciers faster, without adequate snowfall & low winter temps to slow this glacial decrease.
The result is that there is no difference in regional cloud cover trends, neither of
precipitation,
with increasing contamination and that the contaminated area has more dimming, but warmed more than the
less contaminated area.
Based on these figures, I suppose that the West Greenland ice melting was larger in the 1930 - 1950 period than in the 1985 - 2005 period... Alternative explanations may be that the Greenland ice melting has nothing to do
with temperature, but
with more insolation (
less clouds),
less precipitation, more soot deposit,...
Re: 115 Correction — The error would be
less with larger gage openings like the 8 (the 12 in message 115 was incorrect) inch
precipitation gages used by government agencies.
4) Actually, Antarctica (168 mm year continental average) does recieve
less precipitation than the Arctic (< 500 mm per year average),
with the highest most central regions of Antarctica receiving 50 mm per year compared to < 100 to 200 mm per year for central Greenland (described as the driest part of the Arctic).
It would result in a * reduced * rate of cooling
with height and therefore, arguably,
less precipitation.
Snowfall varies across the region, comprising
less than 10 % of total
precipitation in the south, to more than half in the north,
with as much as two inches of water available in the snowpack at the beginning of spring melt in the northern reaches of the river basins.81 When this amount of snowmelt is combined
with heavy rainfall, the resulting flooding can be widespread and catastrophic (see «Cedar Rapids: A Tale of Vulnerability and Response»).82 Historical observations indicate declines in the frequency of high magnitude snowfall years over much of the Midwest, 83 but an increase in lake effect snowfall.61 These divergent trends and their inverse relationships
with air temperatures make overall projections of regional impacts of the associated snowmelt extremely difficult.
For the entire Northern Hemisphere, there is evidence of an increase in both storm frequency and intensity during the cold season since 1950,1
with storm tracks having shifted slightly towards the poles.2, 3 Extremely heavy snowstorms increased in number during the last century in northern and eastern parts of the United States, but have been
less frequent since 2000.11,15 Total seasonal snowfall has generally decreased in southern and some western areas, 16 increased in the northern Great Plains and Great Lakes region, 16,17 and not changed in other areas, such as the Sierra Nevada, although snow is melting earlier in the year and more
precipitation is falling as rain versus snow.18 Very snowy winters have generally been decreasing in frequency in most regions over the last 10 to 20 years, although the Northeast has been seeing a normal number of such winters.19 Heavier - than - normal snowfalls recently observed in the Midwest and Northeast U.S. in some years,
with little snow in other years, are consistent
with indications of increased blocking (a large scale pressure pattern
with little or no movement) of the wintertime circulation of the Northern Hemisphere.5 However, conclusions about trends in blocking have been found to depend on the method of analysis, 6 so the assessment and attribution of trends in blocking remains an active research area.
Bottom right: change in the average maximum number of consecutive days each year
with less than 0.01 inches of
precipitation.
To the north, in Montana, January is typically one of the drier months of the year
with normal
precipitation totals
less than 1 in (25 mm).
Following a wet December, drier to much drier than normal conditions returned to California, Nevada, and Oregon this month,
with precipitation less than 50 % of normal across large portions of these states.
The principal scientific objective is to make global SSS measurements over the ice - free oceans
with 150 - km spatial resolution, and to achieve a measurement error
less than 0.2 (PSS - 78 [practical salinity scale of 1978]-RRB- on a 30 - day time scale, taking into account all sensors and geophysical random errors and biases.Salinity is indeed a key indicator of the strength of the hydrologic cycle because it tracks the differences created by varying evaporation and
precipitation, runoff, and ice processes.
With some exceptions, the tropics will likely receive
less rain (orange) as the planet warms, while the polar regions will receive more
precipitation (green).
Snowpack is melting earlier as winter and spring temperatures rise, and in most states an increasing percentage of winter
precipitation is falling as rain, meaning there is often
less snowpack to begin
with.
Climatic variability in summer is projected to increase,
with southern Europe experiencing more heat,
less precipitation, and more frequent droughts — yet heavier rainstorms when it does rain.23 Northern Europe can expect more overall
precipitation.21 Smog is also expected to rise — unless we reduce our use of fossil fuels.28, 29,30,31
The widespread trend of increasing heavy downpours is expected to continue,
with precipitation becoming
less frequent but more intense.13, 14,15,16 The patterns of the projected changes of
precipitation do not contain the spatial details that characterize observed
precipitation, especially in mountainous terrain, because the projections are averages from multiple models and because the effective resolution of global climate models is roughly 100 - 200 miles.
Overhead, matched -
precipitation rotor systems are the best for irrigating green roofs, and they do a better job
with less water than drip or sub irrigation methods.
According to Neilson, the latest models suggest that parts of the US are experiencing longer - term
precipitation patterns,
with less year - to - year variability but several wet years in a row followed by several years that are drier than normal.
Previous studies on the modification of
precipitation trends by quantile mapping have focused on mean quantities,
with less attention paid to extremes.
Evidence for widespread drought intensification is
less clear and inherently difficult to confirm
with available data because of the increase of time - integrated
precipitation at most locations other than the subtropics.
One suggestion is that a warmer climate would have increased
precipitation efficiency, causing more moisture to rain out,
with less detrainment and a smaller area of upper - level cloud cover, limiting the positive longwave forcing (Lindzen et al. 2001).
By 2080 the prediction is that average temperatures could be 5 - 9 Fahrenheit warmer than they are now
with more
precipitation in the winter and sprint and
less in summer.
A hot - dry climate is defined as region that receives
less than 20 inches (50 cm) of annual
precipitation with approximately 6,300 cooling degree days (50 degrees F basis)[3,500 cooling degree days (10 degrees C basis)-RSB- or greater and where the monthly average outdoor temperature remains above 45 degrees F (7 degrees C) throughout the year.
Those who like to check under the hood and kick the tires will find a tiny increase in
precipitation over the 240 - year record,
with an interesting smoothing of
precipitation through the year - that is, there's been a little more rain in the drier December through May half and a little
less in the soggier June through November half of the year.
«Within our lifetime, winters in Minnesota will become more like winters in Chicago — warmer
with less snow and more
precipitation coming as rain.»
It should also be possible to get
less snow
with the same amount of
precipitation if e.g. the day - night variation increases, in that snow melts during the heat of the day and even if the cold of the night averages out the temperature, the added cold can not remake the lost snow.
In the lower left graph, consecutive dry days are defined as the annual maximum number of consecutive days
with less than 0.01 inches of
precipitation.
Mixed - Humid - A mixed - humid and warm - humid climate is defined as a region that receives more than 20 inches of annual
precipitation with approximately 4,500 cooling degree days (50 °F basis) or greater and
less than approximately 6,300 cooling degree days (50 °F basis) and
less than approximately 5,400 heating degree days (65 °F basis) and where the average monthly outdoor temperature drops below 45 °F during the winter months.
A warm - dry and mixed - dry climate is defined as a region that receives
less than 20 inches of annual
precipitation with approximately 4,500 cooling degree days (50 °F basis) or greater and
less than approximately 6,300 cooling degree days (50 °F basis) and
less than approximately 5,400 heating degree days (65 °F basis) and where the average monthly outdoor temperature drops below 45 °F during the winter months.