Not exact matches
«According to climate predictions, annual
precipitation is likely to
decrease in the Southwest but increase in the eastern United States during the 21st century, therefore, the observed diverse trends of surface water body areas since 1984 could continue to
occur in the future,» said Xiao.
Statewide
precipitation has
decreased in winter (0.14 inches / decade -LSB--0.36 cm / decade]-RRB- since 1950, but no significant change has
occurred in annual mean
precipitation, probably because of very slight increases in spring and fall
precipitation.
This is projected to
occur even in regions where total
precipitation is projected to
decrease, such as the Southwest.1, 7,2
The number of stations reflecting a locally significant increase in the proportion of total annual
precipitation occurring in the upper five percentiles of daily
precipitation totals outweighs the number of stations with significantly
decreasing trends by more than 3 to 1 (Figure 2.36 c).
This can
occur when the probability of
precipitation (the number of events)
decreases, or if the shape of the
precipitation distribution changes, but this latter situation is less likely (Buffoni et al., 1999; Groisman et al., 1999; Brunetti et al., 2000a, b).
Where
precipitation decreases were projected, the results were more complex due largely to interactions between plant biomass, runoff, and erosion, and either increases or
decreases in overall erosion could
occur.
«For the high emissions scenario, it is likely that the frequency of hot days will increase by a factor of 10 in most regions of the world», said Thomas Stocker the other Co-chair of Working Group I. «Likewise, heavy
precipitation will
occur more often, and the wind speed of tropical cyclones will increase while their number will likely remain constant or
decrease».
What the report says about
precipitation, floods, and climate change: Detectable changes in flood frequency have
occurred in parts of the United States, with a mix of increases and
decreases in different regions.
Agricultural droughts can
occur for a variety of reasons, including low
precipitation, the timing of water availability, or
decreased access to water supplies.
Several studies focused on the Colorado River basin showed that annual runoff reductions in a warmer western U.S. climate
occur through a combination of evapotranspiration increases and
precipitation decreases, with the overall reduction in river flow exacerbated by human demands on the water supply.
Areas experiencing large
decreases in
precipitation are evident in both DJF and JJA, in both the high - end and non-high-end members, and
occur between 50 ° N and 50 ° S.