Meridional Gulf Stream Shifts Can Influence Wintertime Variability in the North Atlantic Storm Track and Greenland Blocking

Abstract After leaving the U.S. East Coast, the northward flowing Gulf Stream (GS) becomes a zonal jet and carries along its frontal characteristics of strong flow and sea surface temperature gradients into the North Atlantic at midlatitudes. The separation location where it leaves the coast is also...

وصف كامل

التفاصيل البيبلوغرافية
الحاوية / القاعدة:Geophysical Research Letters
المؤلفون الرئيسيون: Terrence M. Joyce, Young‐Oh Kwon, Hyodae Seo, Caroline C. Ummenhofer
التنسيق: مقال
اللغة:الإنجليزية
منشور في: Wiley 2019-02-01
الموضوعات:
Gulf Stream path changes
wintertime atmospheric storm track
Greenland blocking
intrerannual variability
الوصول للمادة أونلاين:https://doi.org/10.1029/2018GL081087

الانترنت

https://doi.org/10.1029/2018GL081087

مواد مشابهة