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Process-driven improvements to hurricane intensity and storm surge forecasts in the mid-atlantic bight: Lessons learned from hurricanes irene and sandy

机译:在大西洋中大西洋中飓风强度和风暴浪涌预测的过程驱动的改善:从飓风艾琳和桑迪的经验教训

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The coastal northeast United States was heavily impacted by hurricanes Irene and Sandy. Track forecasts for both hurricanes were quite accurate days in advance. Intensity forecasts, however, were less accurate, with the intensity of Irene significantly over-predicted, and the rapid acceleration and intensification of Sandy just before landfall under-predicted. By operating a regional component of the Integrated Ocean Observing System (IOOS), we observed each hurricane's impact on the ocean in real-time, and we studied the impacted ocean's influence on each hurricane's intensity. Summertime conditions on the wide Mid-Atlantic continental shelf consist of a stratified water column with a thin (10m-20m) warm surface layer (24–26C) covering bottom Cold Pool water (8–10C). As the leading edge of Irene tracked along the coast, real-time temperature profiles from an underwater glider documented the mixing and broadening of the thermocline that rapidly cooled the surface by up to 8C, well before the eye passed over. Atmospheric forecast sensitivity studies indicate that the over prediction of intensity in Irene could be eliminated using the observed colder surface waters. In contrast, Hurricane Sandy arrived in the late Fall of 2012 after seasonal cooling had already deepened and decreased surface layer ocean temperatures by 8C. The thinner layer of cold bottom water still remaining before Sandy was forced offshore by downwelling favorable winds, resulting in little change in ocean surface temperature as Sandy crossed and mixed the shelf waters. Atmospheric sensitivity studies indicate that because there was little ocean cooling, there was little reduction in hurricane intensity as Sandy came ashore. Results from Irene and Sandy illustrate the important role of the U.S. IOOS in providing the best estimate of the rapidly evolving ocean conditions to atmospheric modelers forecasting the intensity of hurricanes. Data from IOOS may enable improved hurricane - orecasting in the future.
机译:美国沿海东北部受到飓风艾琳和沙质的影响。飓风的跟踪预测提前完全准确。然而,强度预测不太准确,艾琳强度显着过度预测,并在登陆之前的桑迪快速加速和加强桑迪。通过经营综合海洋观测系统(IOOS)的区域组成部分,我们实时观察了每个飓风对海洋的影响,我们研究了对每个飓风的强度的影响。夏季地大陆架上的夏季条件包括具有薄(10m-20m)暖表面层(24-26℃)的分层水柱,覆盖底部冷水池水(8-10℃)。作为沿着海岸追踪的艾琳的前缘,水下滑翔机的实时温度曲线记录了热量下划线的混合和扩展,在眼睛通过之前快速地将表面迅速冷却到8C。大气预测敏感性研究表明,使用观察到的更冷的表面水可以消除过度预测伊戒强度。相比之下,飓风桑迪在季节性冷却后达到2012年下秋天,已经加深了8℃的表面层海洋温度下降。在桑迪居住的良好风中被迫剩下的含有较薄的冷底水层仍然剩下的剩余的良好风,导致海面温度的变化很小,因为桑迪交叉并混合了货架水。大气敏感性研究表明,由于海洋冷却很小,飓风强度几乎没有减少,因为桑迪岸上岸上。伊琳和桑迪的结果说明了美国iOOS在为大气建模仪提供了预测飓风强度的迅速发展的海洋状况方面的最佳作用。来自ioos的数据可能会在未来提高飓风 - orecasting。

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