Research Article

Drought and Wetness Variability and the Respective Contribution of Temperature and Precipitation in the Qinghai-Tibetan Plateau

Figure 6

The respective contribution rate of the precipitation and temperature variability to the SPEI trend in the QTP. (a) and (b) are the contribution rates of the precipitation and temperature variability in the regions tending to be drier, and (c) and (d) are the contribution rates in the regions tending to be wetter. (a) Cr_temperature. (b) Cr_precipitation. (c) Cr_temperature. (d) Cr_precipitation.
(a)
(b)
(c)
(d)