Not exact matches
Empirical studies of forests across Alaska show that North America's white spruce require at least 280 millimeters (11 inches) of
precipitation each year, a number that rises if
mean summer temperatures are higher than 15.5 degrees Celsius (roughly 60 degrees Fahrenheit).
Earlier spring - like weather
means more of the
precipitation will not be stored as long in the mountains, which can result in lower river and reservoir levels during late
summer and early fall.
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
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.
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.»
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).
According to data from the Salekhard weather station the recent
mean air
summer temperature was 0.9 °C higher and winter was 1.2 °C higher than between 1883 and 1919; and the amount of
precipitation also increased by 32 mm in
summer and by 46 mm in winter.
First point, a long known fact is that the upper midwest (
meaning, the northern tier, west of the 25 inch annual average rainfall line) has a
Summer precipitation maximum, so dry winters can indeed be expected.
In mountain regions that are warming, as most are, a larger fraction of
precipitation falls as rain rather than as snow, which
means lower stream flows in spring and
summer.
Figure 3, above: Regional time series of boreal
summer (JJA) irrigation, ensemble -
mean temperature anomalies, and ensemble -
mean precipitation anomalies for Western North America (130 ° W - 100 ° W, 30 ° N - 50 ° N), India (68 ° E-88 ° E, 8 ° N -36 ° N), and China (98 ° E-122 ° E, 22 ° N - 42 ° N).