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首页> 外文期刊>Frontiers in Physics >A model study of the seasonality of sea surface temperature and circulation in the Atlantic North-eastern Tropical Upwelling System
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A model study of the seasonality of sea surface temperature and circulation in the Atlantic North-eastern Tropical Upwelling System

机译:大西洋东北热带上升流系统海表温度和环流季节性的模型研究

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The climatological seasonal cycle of the sea surface temperature (SST) in the north-eastern tropical Atlantic (7-25°N, 26-12°W) is studied using a mixed layer heat budget in a regional ocean general circulation model. The region, which experiences one of the larger SST cycle in the tropics, forms the main part of the Guinea Gyre. It is characterized by a seasonally varying open ocean and coastal upwelling system, driven by the movements of the intertropical convergence zone (ITCZ). The model annual mean heat budget has two regimes schematically. South of roughly 12°N, advection of equatorial waters, mostly warm, and warming by vertical mixing, is balanced by net air-sea flux. In the rest of the domain, a cooling by vertical mixing, reinforced by advection at the coast, is balanced by the air-sea fluxes. Regarding the seasonal cycle, within a narrow continental band, in zonal mean, the SST early decrease (from September, depending on latitude, until December) is driven by upwelling dynamics off Senegal and Mauritania (15°-20°N), and instead by air-sea fluxes north and south of these latitudes. Paradoxically, the later peaks of upwelling intensity (from March to July, with increasing latitude) essentially damp the warming phase, driven by air-sea fluxes. The open ocean cycle to the west, is entirely driven by the seasonal net air-sea fluxes. The oceanic processes significantly oppose it, but for winter north of ~18°N. Vertical mixing in summer-autumn tends to cool (warm) the surface north (south) of the ITCZ, and advective cooling or warming by the geostrophic Guinea Gyre currents and the Ekman drift. This analysis supports previous findings on the importance of air-sea fluxes offshore. It mainly offers quantitative elements on the modulation of the SST seasonal cycle by the ocean circulation, and particularly by the upwelling dynamics. Keywords: SST, upwelling, circulation, heat budget, observations, modeling.
机译:在区域海洋总环流模型中,使用混合层热收支研究了东北热带大西洋(7-25°N,26-12°W)海表温度(SST)的气候季节性周期。该地区是热带地区较大的SST周期之一,是几内亚回旋区的主要部分。它的特点是受热带辐合带(ITCZ)的运动驱动,季节性变化的开放海洋和沿海上升流系统。该模型的年平均热量预算示意性地具有两个机制。在大约12°N以南,赤道水的平流(大部分为温暖)和垂直混合引起的变暖与净海气通量平衡。在该区域的其余部分,通过垂直混合进行的冷却,再加上海岸的对流增强,通过海气通量来平衡。关于季节周期,在一个狭窄的大陆带内,以区域平均数表示,SST的早期下降(从9月开始,取决于纬度,直到12月)是由塞内加尔和毛里塔尼亚(北纬15°-20°)上升的动力驱动的,而相反这些纬度以北和以南的海气通量。矛盾的是,上升气流强度的后期峰值(从3月到7月,随着纬度的增加)基本上抑制了由海气通量驱动的升温阶段。西部的公海周期完全由季节性的海-气净通量驱动。海洋过程强烈反对它,但在冬季〜18°N以北。夏季-秋季的垂直混合趋向于使ITCZ北部(南部)的地表变凉(变暖),并且由于地转几内亚涡流和Ekman漂移而导致对流冷却或变暖。该分析支持了先前关于海上气海通量重要性的发现。它主要通过海洋环流,尤其是上升流动力学,提供了关于SST季节周期调节的定量要素。关键词:SST,上升流,环流,热量收支,观测,建模。

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