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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Impact of permafrost degradation on the extreme increase of dissolved iron concentration in the Amur river during 1995–1997

Fig. 2

Interannual variations of climate variables in the Amur River basin. Regional mean a annual air temperature (Ta), b accumulated temperature (AT), and c late summer (July, August, September; JAS) mean net precipitation (P − E) in the NE-Amur (red), the NW-Amur (green), and the S-Amur (blue). In c, P − E values above the black dotted line indicate net water gain as a result of infiltration and values below the line indicate net water loss as a result of evapotranspiration

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