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Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989.

机译:1988年9月17日至1989年1月7日,东方北极协调实验(CEAREX)第一阶段的气象特征。

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摘要

The synoptic and mesoscale meteorological conditions were analyzed for Phase I ofthe Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7January 1989. Meteorological observations from a research ship (R/V Polarbjoern), anarray of drifting buoys and satellite imagery from DMSP and NOAA satellites were theprimary tools for analysis. Several short periods of high cyclone activity followed bylong periods of high pressure dominated the weather pattern in the eastern Arctic Oceanfrom Greenland to Novaya Zemlya for this period. Two case studies are presented. Aninfrequent cyclogenesis event that formed within a strong baroclinic zone over Arcticpack ice was observed in a "baroclinic leaf on satellite imagery. Ship and drifting buoyobservations provided critical insight to the location and intensity of the "leafs" subsequentvertical development to the surface. In the second study, a boundary layer frontwas observed in the East Greenland Sea by satellite imagery. The front then movednortheast into Fram Strait and a polar low formed at the northern end of the front. Theevent lasted less than 24 h and would not have been observed except through satelliteimagery.
机译:分析了1988年9月17日至1989年1月7日东部协调北极实验(CEAREX)第一阶段的天气和中尺度气象条件。研究船(R / V Polarbjoern)的气象观测结果,一系列浮标和DMSP和NOAA卫星是进行分析的主要工具。在这段时期内,从格陵兰岛到诺瓦亚·泽姆利亚,北冰洋东部的几个短时期的高气旋活动以及随后的长时期的高压主导了天气模式。介绍了两个案例研究。在“卫星图像上的斜压叶片上,观察到了在北极圈冰上强斜压带内形成的罕见环回事件。船舶浮标和漂流浮标观测为随后垂直发展到地表的”叶片”的位置和强度提供了关键的见识。研究表明,通过卫星图像在东格陵兰海中观察到了边界层前缘,然后该前缘向北移动到弗拉姆海峡,并在该前缘的北端形成了一个极地低压,事件持续了不到24小时,除非经过卫星图像。

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    Hamilton Stephanie W.;

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  • 年度 1991
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