Not exact matches
Under various climate and land - use scenarios, coniferous stands are expected to lose 71 percent to 100 percent of their current range to deciduous stands
across New England by 2085, particularly in Vermont, New Hampshire and Maine, due to
increased temperature and
precipitation and changes in timber harvesting.
Over the 121 - year period of record,
precipitation across the CONUS has
increased at an average rate of 0.16 inch per decade.
has decreased in winter, but no significant change in annual mean
precipitation potentially because of very slight
increases in spring and fall
precipitation;
precipitation is projected to
increase across Montana, primarily in spring; slight decrease in summer
precipitation; variability of
precipitation year - to - year projected to
increase
The majority of models suggest a slight
increase in total average annual
precipitation across the state, largely occurring in spring, particularly in the northwest.
Half the
increase in urban land
across the world over the next 20 years will occur in Asia, with the most extensive change expected to take place in India and China Urban areas modify their local and regional climate through the urban heat island effect and by altering
precipitation patterns, which together will have significant impacts on net primary production, ecos...
We know that
precipitation intensity has been
increasing (the amount of rain that falls in the most intense events)
across the northern hemisphere — this was clear in the literature even before the Pall et al paper.
doi: 10.1130 / G23261A.1 v. 35 no. 3 p. 215 - 218 Abrupt
increase in seasonal extreme
precipitation at the Paleocene - Eocene boundary B Schmitz, V Pujalte — Geology, 2007 — geology.gsapubs.org A prominent
increase in atmospheric CO2 at the Paleocene - Eocene boundary, ca. 55 Ma, led to the warmest Earth of the Cenozoic for ∼ 100 ky High - resolution studies of continental flood - plain sediment records
across this boundary....
«During November 2011 - January 2012, there is an
increased chance of above - average temperatures
across the south - central U.S. with the odds favoring below - average temperatures over the north - central U.S.. Also, above - average
precipitation is favored
across the northern tier of states, excluding New England, and drier - than - average conditions are more probable
across the southern tier of the U.S. (see 3 - month seasonal outlook released on 20 October 2011).»
It may well be that the West will luck out as rising greenhouse gases induce an equatorial warming, or an El Niño - like response, and the resulting circulation changes
increase precipitation across the mid-latitudes.
He cited a recent analysis by scientists from the National Climatic Data Center that confirmed earlier studies showing a substantial
increase already in the intensity of
precipitation across the United States, interspersed by longer dry spells.
The Candadian model projects decreases in
precipitation across the eastern half of the US while the Hadley model projects
increases.
Increases in
precipitation at high latitudes in both seasons are very consistent
across models.
As for how this could be — and in light of the findings of the references listed above — Rankl et al. reasoned that «considering
increasing precipitation in winter and decreasing summer mean and minimum temperatures
across the upper Indus Basin since the 1960s,» plus the «short response times of small glaciers,» it is only logical to conclude that these facts «suggest a shift from negative to balanced or positive mass budgets in the 1980s or 1990s or even earlier, induced by changing climatic conditions since the 1960s.»
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.
2: Our Changing Climate, Key Message 5).2 Regional climate models (RCMs) using the same emissions scenario also project
increased spring
precipitation (9 % in 2041 - 2062 relative to 1979 - 2000) and decreased summer
precipitation (by an average of about 8 % in 2041 - 2062 relative to 1979 - 2000) particularly in the southern portions of the Midwest.12
Increases in the frequency and intensity of extreme precipitation are projected across the entire region in both GCM and RCM simulations (Figure 18.6), and these increases are generally larger than the projected changes in average precipitat
Increases in the frequency and intensity of extreme
precipitation are projected
across the entire region in both GCM and RCM simulations (Figure 18.6), and these
increases are generally larger than the projected changes in average precipitat
increases are generally larger than the projected changes in average
precipitation.12, 2
The pattern of change for the wettest day of the year is projected to roughly follow that of the average
precipitation, with both
increases and decreases
across the U.S. Extreme hydrologic events are projected to
increase over most of the U.S.
Both (top right and bottom left) indicate that heavy
precipitation events will
increase in intensity in the future
across the Midwest.
Hundreds of millions of people in urban areas
across the world will be affected by rising sea levels,
increased precipitation, inland floods, more frequent and stronger cyclones and storms, and periods of more extreme heat and cold.
SRM on the other hand would merely mask temperature
increases, with limited effects on ocean acidification, and would create novel climate regimes
across significant areas of the world, with new patterns and levels of
precipitation.
Depending on winter
precipitation and the forest treatment schedule, mean annual
increases in runoff from thinning of ponderosa forests
across the Salt - Verde watersheds ranged from 4.76 to 15.0 million m3 (3,860 — 12,200 acre - feet) over a 35 - year treatment period, 6.18 to 23.4 million m3 (5,010 to 19,000 acre - feet) over 25 years, and 9.23 to 42.8 million m3 (7,480 to 34,700 acre - feet) over 15 years (Table 2).
Overall, it is likely that there has been a 2 to 4 %
increase in the number of heavy
precipitation events when averaged
across the mid - and high latitudes.
It's interesting to note that while the result of a muted
precipitation response to global warming appears to be theoretically sound and robust
across models, satellite observations suggest that
precipitation is
increasing closer to 7 % per K, instead of 3 % per K (Wentz et al 2007).
In agreement with this speculation are climate projections suggesting
increased flood magnitude in the future
across the Southwest, despite reduced mean
precipitation amounts [4].
Since 1895,
precipitation across the CONUS has
increased at an average rate of 0.16 inch per decade.
According to the National Climate Assessment, average rainfall during heavy
precipitation events
across the Northeast, Midwest and Great Plains has
increased by 30 percent since 1991.
«[C] ommunities
across the Nation are already experiencing a range of climatic changes, including more frequent and extreme
precipitation events, longer wildfire seasons, reduced snowpack, extreme heat events,
increasing ocean temperatures, and rising sea levels,» the report says.
One sentence summary: A strengthened subtropical jet stream — which is the primary means by which El Niño brings
increased precipitation to California — is unlikely to occur prior to winter due to the intrinsic seasonal cycle of temperature variations
across the Pacific Basin.
A warmer atmosphere drives more extreme
precipitation across all storm types, which in turn
increases the the risk of flooding.
Consistent with the predicted impacts of global warming, we found that storms with extreme
precipitation have
increased in frequency by 24 percent
across the continental United States since 1948.
We know that
precipitation intensity has been
increasing (the amount of rain that falls in the most intense events)
across the northern hemisphere — === Really, more precip?
A large ensemble of climate model simulations suggests that the frequency of extreme wet - to - dry
precipitation events will
increase by 25 % to 100 %
across California due to anthropogenic forcing.
If the emissions that cause global warming continue unabated, scientists expect the amount of rainfall during the heaviest
precipitation events
across country to
increase more than 40 percent by the end of the century.
(Drought expanded
across the Central U.S. last week as
precipitation deficits there
increased.
Mean
precipitation has
increased across Canada by about 12 % in the last 50 years, meaning we now experience 20 additional days of rain.3