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.