ملخص
During two cruises to the Greenland Sea in winter 2001 a narrow convective chimney extending from the surface to a depth exceeding 2400 meters was is covered and mapped in detail. The feature was observed to be stable over a period of a month and its centre moved only 700 m in that time; its diameter was only 10 km. At a time when deep convection is thought to have ceased in the Greenland Sea the existence of this feature is a challenge to our understanding of the causes and impacts of open ocean winter convection.
| اللغة الأصلية | English |
|---|---|
| عنوان منشور المضيف | Norwegian Ocean Climate Project |
| العنوان الفرعي لمنشور المضيف | Technical Report No. 3 |
| ناشر | University of Berlin |
| الصفحات | 35-40 |
| عدد الصفحات | 6 |
| طبعة | No. 3 |
| حالة النشر | Published - 2002 |
| الحدث | NOClim Science meeting 2002 - Clarion Hotel Oslo Airport, Gardermoen, Norway المدة: ١٣ مايو ٢٠٠٢ → ١٥ مايو ٢٠٠٢ https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf |
سلسلة المنشورات
| الاسم | Norwegian Ocean Climate Project. Technical Report |
|---|---|
| ناشر | University of Bergen |
Conference
| Conference | NOClim Science meeting 2002 |
|---|---|
| الدولة/الإقليم | Norway |
| المدينة | Gardermoen |
| المدة | ١٣/٠٥/٠٢ → ١٥/٠٥/٠٢ |
| عنوان الإنترنت |
بصمة
أدرس بدقة موضوعات البحث “A Deep Convective Chimney in the Winter Greenland Sea (Wadhams, Hansen and Wilkinson )'. فهما يشكلان معًا بصمة فريدة.قم بذكر هذا
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