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A 332-year dendrohydrological record of regionalized mean summer streamflow for four watersheds is analyzed to place recent drought magnitudes in a long-term perspective.
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Seasonally, temperature has a strong effect on streamflow in autumn and winter, while summer streamflow appears more sensitive to changes in precipitation.
And I mean this month.
I mean, last year was last year.
Do you mean today?
At the average monthly time-scale, a majority of the hydrologic projections varied in peak streamflow timing, peak streamflow magnitude, summer streamflows, as well as overall increases or decreases compared to the historical monthly streamflows.
Moreover, we show that the winter streamflow is very sensitive to the influence of winter temperatures.
Aujourd'hui means "today".
While the distribution of mean monthly precipitation is uniform throughout the year over most of the eastern United States (except peninsular Florida), mean monthly streamflow exhibits pronounced seasonality with peak runoff occurring during the winter early springg) over the Southeast (Mid-Atlantic and Northeast) regions.
Streams represented by the first annual factor occurred in southern Wisconsin and the lower peninsula of Michigan, and exhibited a linear increase in mean annual streamflow over the 33 year period caused by increased autumn and winter runoff.
For the whole Poyang Lake catchment, the variations of mean annual streamflow in 1970 2007 were primarily affected by climate change with reference to 1960s, while human activities played a complementary role.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com