The meridional variability of the components of moisture exchange between the ocean and the atmosphere in the northern Atlantic
Publish place: Fifth International Conference on Persian Gulf Oceanography
Publish Year: 1400
نوع سند: مقاله کنفرانسی
زبان: English
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شناسه ملی سند علمی:
ICPGO05_028
تاریخ نمایه سازی: 19 خرداد 1401
Abstract:
Output from Reanalysis ۲ is used to express the temporal and spatial variations of rainfall, evaporation on the North Atlantic. This archive has been used for the years ۱۹۸۰-۲۰۱۶ within ۳۰۰N-۷۰۰N. The difference between E and P is the net freshwater flux, which directly affects salinity and thus classifies the ocean surface layers. In mean annual, P exceeds E in the North Atlantic poleward of ۵۰۰N; E exceeds P between ۲۰۰N and ۵۰۰N as well as in the eastern Atlantic Ocean (۱۰۰N-۳۵۰N). Seasonal changes are significant among the regions: s: P and E both peak during the cold period (October-March) in the subpolar region, also P and E values are close in the warm cold period at latitude ۴۱۰N, so that in the warm period, their difference approaches zero.
Keywords:
Authors
Martha Abbasi Moheb
Hydrometeorological University, St. Petersburg, Russia,
V.N. Malinin
Hydrometeorological University, St. Petersburg, Russia,