1> (from surface to 100 hPa) is complicated, displaying noticeable regionality, i.e., the heat source changes faster in the western than in the eastern QTP, with the western source considerably stronger in April - August, and intensified quickly enough to show a 200 W/m2 center in May, one month ahead of the eastern source. When July comes the regional heat source begins to weaken towards the south, during which the western source weakens faster, changing to a cold source in October, again one month earlier compared to the eastern counterpart; 4) since 1979 the seasonal variability of the heat source has shown climate transition signals, as clearly seen in 1990/91. |
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Climatology
Troposphere
Climate change
Solids
Atmospheric modeling
Atmospheric sciences
Picosecond phenomena