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首页> 外文期刊>Journal of Climate >Rewriting the climatology of the tropical North Atlantic and Caribbean Sea atmosphere.
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Rewriting the climatology of the tropical North Atlantic and Caribbean Sea atmosphere.

机译:重写北大西洋和加勒比海热带大气的气候学。

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The Jordan mean tropical sounding has provided a benchmark reference for representing the climatology of the tropical North Atlantic and Caribbean Sea atmosphere for over 50 years. However, recent observations and studies have suggested that during the months of the North Atlantic hurricane season, this region of the world is affected by multiple air masses with very distinct thermodynamic and kinematic characteristics. This study examined ~6000 rawinsonde observations from the Caribbean Sea region taken during the core months (July-October) of the 1995-2002 hurricane seasons. It was found that single mean soundings created from this new dataset were very similar to C. L. Jordan's 1958 sounding work. However, recently developed multispectral satellite imagery that can track low- to midlevel dry air masses indicated that the 1995-2002 hurricane season dataset (and likely Jordan's dataset as well) was dominated by three distinct air masses: moist tropical (MT), Saharan air layer (SAL), and midlatitude dry air intrusions (MLDAIs). Findings suggest that each sounding is associated with unique thermodynamic, kinematic, stability, and mean sea level pressure characteristics and that none of these soundings is particularly well represented by a single mean sounding such as Jordan's. This work presents three new mean tropical soundings (MT, SAL, and MLDAI) for the tropical North Atlantic Ocean and Caribbean Sea region and includes information on their temporal variability, thermodynamics, winds, wind shear, stability, total precipitable water, and mean sea level pressure attributes. It is concluded that the new MT, SAL, and MLDAI soundings presented here provide a more robust depiction of the tropical North Atlantic and Caribbean Sea atmosphere during the Atlantic hurricane season and should replace the Jordan mean tropical sounding as the new benchmark soundings for this part of the world.Digital Object Identifier http://dx.doi.org/10.1175/2010JCLI3496.1
机译:约旦的平均热带测深为代表北大西洋和加勒比海热带气候50多年来的气候学提供了基准。但是,最近的观察和研究表明,在北大西洋飓风季节的几个月中,世界这个地区受到多种气团的影响,这些气团具有非常不同的热力学和运动学特征。这项研究检查了在1995-2002年飓风季节的核心月份(七月至十月)从加勒比海地区获得的大约6000枚Rawinsonde观测值。结果发现,从这个新数据集创建的单一均值测深与C. L. Jordan 1958年的测深工作非常相似。但是,最近开发的可跟踪中低空干燥空气质量的多光谱卫星图像显示,1995-2002年飓风季节数据集(可能还有约旦的数据集)主要由三个不同的空气质量控制:潮湿的热带(MT),撒哈拉沙漠的空气层(SAL)和中纬度干空气入侵(MLDAI)。研究结果表明,每种测深都具有独特的热力学,运动学,稳定性和平均海平面压力特征,而且这些测深中没有一个可以用单一的平均测深来很好地代表,例如约旦。这项工作为热带北大西洋和加勒比海地区提供了三种新的平均热带测深(MT,SAL和MLDAI),并包括了有关它们的时间变化,热力学,风,风切变,稳定性,总可沉淀水和平均海域的信息。水平压力属性。结论是,此处介绍的新的MT,SAL和MLDAI测深提供了对大西洋飓风季节期间北大西洋和加勒比海热带大气的更生动描述,并且应取代约旦的平均热带测深作为该部分的新基准测深数字对象标识符http://dx.doi.org/10.1175/2010JCLI3496.1

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