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The continuous winter to spring drought is one of the main causes of wildfires in Yunnan (Chen et al. 2012).
Since 2000, droughts from September to December and January to March have been more severe compared with historical records, which has led to a more frequent and intense winter to spring drought and increased wildfires in Yunnan.
Since the first appearance of WNV in Florida during 2001, the hydrologic pattern of spring drought followed by summer wetting has not occurred.
This seasonality, being consistent with the observed hydro-climate trend in the last 40 50 years (Qin et al., 2010b), would potentially result in more frequencies of spring drought events and summer flooding.
The shrinkage this year is due to spring drought conditions in the Mississippi Basin, which reduced the nutrient flows that fuel algal blooms in the gulf.
Noormets et al. (2008) reported that a spring drought might suppress forest canopy development such as leaf sprout and expansion and have long-lasting effects on the forest ecosystem carbon balance.
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Wolf, S. et al. Warm spring reduced carbon cycle impact of the 2012 US summer drought.
While the magnitudes of annual mean streamflow responses are minor, there would be a seasonal shift: drier spring and wetter summer would potentially result in the increasing frequency of spring drought events and summer flooding, and would produce serious challenge for water resources planning and management for Southwest China.
The case study in 2010 spring drought further shows that the spatio-temporal evolutions are modulated by the basin-scale topography.
And the 2002 drought was a doozy.
Then the 1999 drought came".
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