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Towards a Mechanistic Understanding of Precipitation Over the Far Eastern Tropical Pacific and Western Colombia,One of the Rainiest Spots on Earth

机译:对远东热带太平洋和西方哥伦比亚的降水的机制理解,地球上最荒凉的斑点之一

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According to Tropical Rainfall Measuring Mission (TRMM) and Global Precipitation Measurement (GPM) satellite precipitation composites, a broad maritime area over the far eastern tropical Pacific and western Colombia houses one of the rainiest spots on Earth. This study aims to present a suite of mechanistic drivers that help create such a world-record-breaking rainy spot. Previous research has shown that this oceanic and nearly continental precipitation maximum has a strong early morning precipitation peak and a high density of mesoscale convective systems. We examined new and unique observational evidence highlighting the role of both dynamical and thermodynamical drivers in the activation and duration of organized convection. Results showed the existence of a rather large combination of mechanisms, including: (1) dynamics of the Choco (ChocoJet) and Caribbean Low-Level Jets along their confluence zone, including the Panama semi-permanent low; (2) ChocoJet deceleration offshore is favored by land breeze, enhancing the nighttime and early morning low-level convergence; (3) a wind sheared environment that conforms to the long-lived squall line theory;(4) action of mid-level gravity waves, which further support the strong diurnal variability; and (5) mesoscale convective vortices related to subsidence in the stratiform region and top-heavy mass flux profiles. This study emphasizes the multiscale circulation and thermodynamics mechanisms associated with the formation of one of the rainiest spots on Earth and showcases new observations gathered during the Organization of Tropical East Pacific Convection field campaign (OTREC; August-September, 2019) that support the outlined mechanisms.
机译:根据热带降雨测量任务(TRMM)和全球降水测量(GPM)卫星降水复合材料,在远东热带地区和哥伦比亚西部的广泛海洋区域都拥有地球上最雨的斑点之一。本研究旨在展示一套机械司机,有助于创造这样一个世界录制的下雨场所。以前的研究表明,这种海洋和几乎欧式降水最大值具有强烈的清晨降水峰值和高密度的Mescle对流系统。我们检查了新的和独特的观察证据,突出了动态和热力学驱动因子在有组织对流的激活和持续时间中的作用。结果表明,存在相当大的机制组合,包括:(1)Choco(Chocojet)和沿着汇合区的加勒比低级喷气机的动态,包括巴拿马半永久性低; (2)Chocojet Depeleration海上受到土地微风的青睐,增强了夜间和清晨的低级收敛; (3)风剪的环境,符合长寿的Quall线理论;(4)中级重力波的作用,进一步支持强大的昼夜变异性; (5)与层状区域和顶层质量磁通剖面有关的Messcale对流涡旋。本研究强调了与地球上最衰落的最雨量的形成相关的多尺度循环和热力学机制,展示了热带东太平洋对流场运动组织期间聚集的新观测(OTREC; 2019年8月)支持概述机制。

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    《Oceanographic Literature Review》 |2021年第5期|981-982|共2页
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  • 入库时间 2022-08-19 02:27:29

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