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عمران::
عرضی،عرض جغرافیایی
The requirements for meaningful values of EF (positive energy fluxes and 0 # EF # 1; see section 2b) lead to a latitudinal gradient in the number of considered 3-month subsets (Figs. 4a-c).
The latitudinal variations of ET and its components in ERA-Interim/Land (E.
The overall agreement of the latitudinal ET variations (and also the variations of the single ET components) in the different datasets provides confidence that the global patterns of soil moisture-temperature coupling are robust.
The maps reveal a clear latitudinal dependence of the
The results reveal that many re- gions, mostly located in low latitudes, enter the transi- tional regime in the course of the year and about 30%-60% (depending on the dataset) of the latitudinal- corrected global land area (without Greenland and Antarctica) lies in the transitional regime during at least half of the year (Fig. 4).
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