美洲海洋表面温度的季节-年际变化:区域海洋模式系统中的模式相关偏差

IF 0.1
Ana Lucia Caicedo Laurido, Ángel G. Muñoz Solórsano, X. Chourio, Cristian Andrés Tobar Mosquera, Sadid Latandret
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引用次数: 0

摘要

包括墨西哥湾、加勒比海和与中美洲、哥伦比亚和厄瓜多尔接壤的热带太平洋东部的一部分在内的美洲海显示出非常活跃的海洋-陆地-大气相互作用,影响着该区域内外的社会经济活动,而这种相互作用仍然没有得到很好的理解,也没有在最先进的模式中得到很好的体现。在季节-年际时间尺度上,该地理区域变率的主要来源与太平洋和大西洋之间的相互作用有关,涉及El Niño-Southern涛动(ENSO)等海表温度(SST)异常模式,以及与加勒比海低空急流的双峰季节性相关的加勒比地区区域特征。本研究探讨了观测资料中IAS表面温度的季节性至年际异常,以及它们在由气候预报系统再分析(Climate Forecast System Reanalysis)年际强迫使用区域海洋模拟系统(ROMS)进行的允许涡流、1/ 90分辨率模拟中的表现。在这里,不是局部分析模型偏差(即逐个网格盒),而是通过主成分分析进行基于非局部海温模式的诊断。该方法可以确定与西半球暖池、ENSO、美洲海偶极子和其他几种变率模态相关的海温模式的幅度、方差和空间系统误差。这些偏差主要与以下因素有关:地表热通量的误差、对影响加勒比海地表潜冷的海气相互作用的错误描述,以及主要发生在厄瓜多尔海岸和秘鲁北部的地下热分层过于强烈。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seasonal-To-Interannual Variability of Sea-Surface Temperatures in The Inter-Americas Seas: Pattern-Dependent Biases in The Regional Ocean Modeling System
The Inter-Americas Seas (IAS), involving the Gulf of Mexico, the Caribbean and a section of the eastern tropical Pacific Ocean bordering Central America, Colombia and Ecuador, exhibits very active ocean-land-atmosphere interactions that impact socio-economic activities within and beyond the region, and that are still not well understood or represented in state-of-the-art models. On seasonal-to-interannual timescales, the main source of variability of this geographical area is related to interactions between the Pacific and the Atlantic oceans, involving to anomalous sea-surface temperature (SST) patterns like El Niño-Southern Oscillation (ENSO), and regional features in the Caribbean linked to the bi-modal seasonality of the Caribbean Low-Level Jet. This study investigates seasonal-to-interannual IAS surface-temperature anomalies in observations, and their representation in am eddy-permitting, 1/9o-resolution simulation using the Regional Ocean Modeling System (ROMS), interannually-forced by the Climate Forecast System Reanalysis. Here, rather than analyzing model biases locally (i.e., gridbox-by-gridbox), a non-local SST pattern-based diagnostic was conducted via a principal component analysis. The approach allowed to identify magnitude, variance and spatial systematic errors in SST patterns related to the Western Hemisphere Warm Pool, ENSO, the Inter-American Seas Dipole, and several other variability modes. These biases are mainly related to errors in surface heat fluxes, misrepresentation of air-sea interactions impacting surface latent cooling in the Caribbean, and too strong sub-surface thermal stratification, mostly off the coast of Ecuador and northern Peru.
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来源期刊
Avances en Ciencias e Ingenieria
Avances en Ciencias e Ingenieria ENGINEERING, MULTIDISCIPLINARY-
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