Sentences with phrase «summer precipitation changes»

This paper demonstrates there is a glimmer of hope on the horizon for new climate simulation technology to crack the difficult problem of projecting future summer precipitation changes in continental interiors.

Not exact matches

As climate change raises summer temperatures around the world, increases in precipitation could offset drought risk in some regions.
Warmer summers, changing precipitation patterns and a thinning snow pack are already «aridifying» Western forests, University of Montana Professor Steven Running said during a conference here last week.
The study projects that, by 2020 and into the 2080s, Washington will experience higher temperatures, changes in precipitation patterns, and lower summer water supplies.
In 2012, a controversial study challenged previously accepted ideas about the mechanisms through which climate change will affect our weather: Warmer temperatures will result in more heat waves, hotter summers will bring worse droughts, the warmer atmosphere will hold more water, resulting in heavier precipitation and flooding.
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
Wiper blades are cheap, easy to change, and often overlooked, especially if you live in an area that doesn't get much precipitation during the summer months.
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.»
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 precipitation.12, 2
Model projections for precipitation changes are less certain than those for temperature.12, 2 Under a higher emissions scenario (A2), global climate models (GCMs) project average winter and spring precipitation by late this century (2071 - 2099) to increase 10 % to 20 % relative to 1971 - 2000, while changes in summer and fall are not expected to be larger than natural variations.
The precipitation changes probably will lead to «reduced water supplies» in Western reservoirs that rely on snowmelt during the late spring and summer, scientists warn.
Even in areas where precipitation does not decrease, these increases in surface evaporation and loss of water from plants lead to more rapid drying of soils if the effects of higher temperatures are not offset by other changes (such as reduced wind speed or increased humidity).5 As soil dries out, a larger proportion of the incoming heat from the sun goes into heating the soil and adjacent air rather than evaporating its moisture, resulting in hotter summers under drier climatic conditions.6
Ozone depletion in the late twentieth century was the primary driver of the observed poleward shift of the jet during summer, which has been linked to changes in tropospheric and surface temperatures, clouds and cloud radiative effects, and precipitation at both middle and low latitudes.
As the climate of the Pacific Northwest warms, more winter precipitation is falling as rain, compared with historical averages.2 With declining snowpack in Oregon's Cascade Mountains, peak stream flows are occurring earlier, and summer flows are declining.2 These changes are expected to continue as heat - trapping emissions grow, putting more stress on already endangered salmon that return to the Columbia and other rivers in the region to spawn.2
For the 2050s, the range of projected change in the Capital Regional District (CRD) is +1.3 °C to +2.6 °C in summer, +0.8 °C to +2.4 °C in winter, -5 % to +17 % in winter precipitation, and -30 % to +1 % in summer precipitation.
For the 2050s, the range of projected change in Metro Vancouver is +1.4 °C to +2.8 °C in summer, +0.8 °C to +2.7 °C in winter, -5 % to +16 % in winter precipitation, and -25 % to +5 % in summer precipitation.
The δ18O of speleothem calcite at this Puerto Rican location varies primarily in response to changes in the amount of summer - time precipitation.
Glaciers follow an annual cycle, melting in summer and growing in winter owing to seasonal changes in temperature and precipitation.
He said severe effects of climate change on water resources could be seen in shape of changes in precipitation, drastic increasing trends in temperature, hazardous alteration in period of winter and summer, harmful rising in the sea level and depletion of groundwater.
Multi-model mean changes in surface air temperature (°C, left), precipitation (mm day — 1, middle) and sea level pressure (hPa, right) for boreal winter (DJF, top) and summer (JJA, bottom).
This report discusses our current understanding of the mechanisms that link declines in Arctic sea ice cover, loss of high - latitude snow cover, changes in Arctic - region energy fluxes, atmospheric circulation patterns, and the occurrence of extreme weather events; possible implications of more severe loss of summer Arctic sea ice upon weather patterns at lower latitudes; major gaps in our understanding, and observational and / or modeling efforts that are needed to fill those gaps; and current opportunities and limitations for using Arctic sea ice predictions to assess the risk of temperature / precipitation anomalies and extreme weather events over northern continents.
«Climate change could influence monsoon dynamics and cause lower summer precipitation, a delay to the start of the monsoon season and longer breaks between the rainy periods.»
In the video below «Influence of Arctic sea ice on European summer precipitation (2013)», Dr James Screen explains the impacts of climate change on farming and flooding.
It's crucial to note that while overall precipitation is predicted to go up in Canada, that precipitation will come in winter, not in summer during the growing season, says geographer David Sauchyn, a professor at the University of Regina, who recently led a federal government study on the impacts of climate change on the prairies.
In our presentation to the Science Policy Conference of the American Geophysical Union this summer, we even included a table listing the number of years into the future it would be before projected changes in precipitation across the U.S. rose above the level of nature variability.
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