Verification of air/surface humidity differences from AIRS and ERA-Interim in support of turbulent flux estimation in the Arctic
Evaporation from the Arctic Ocean and its marginal seas is essential for air moisture, cloudiness, and precipitation, as well as for the associated feedbacks, which contribute to the Arctic amplification of climate warming. However, evaporation in the Arctic is still associated with large uncertaint...
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Veröffentlicht in: | Journal of geophysical research. Atmospheres 2015-02, Vol.120 (3), p.945-963 |
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Sprache: | eng |
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