Analysis of mesoscale frontal zones of the Norwegian Sea based on satellite observations and reanalysis data in May 2011–2020

A. Konik, O. A. Atadzhanova, E. V. Sentyabov
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Abstract

   The aim of this study is to compare the horizontal temperature gradients calculated based on satellite observations and reanalysis data in the area of mesoscale frontal zones’ surface manifestations, both for the entire Norwegian Sea and during the onset of pelagic fish spawning migrations in May from 2011 to 2020.   Using monthly average temperature data from MODIS/Aqua, GHRSST OSTIA, and CMEMS GLORYS12v1, the fields of monthly and decade-long horizontal gradients on the surface of the Norwegian Sea were derived. A comparison was made between the decade-long temperature gradient estimates and their mean climatic values. The majority of the data show surface manifestations of the main frontal zones in the Norwegian Sea. Validation of temperature fields in the area of the Iceland-Faroe Frontal Zone was conducted based on unique in situ observations. It was demonstrated that for the analysis of the frontal zones in the Norwegian Sea, using the temperature fields of GHRSST OSTIA is most preferable. The obtained physico-geographical characteristics of mesoscale frontal zones could be used to assess their relationship with pelagic fish migrations in the Norwegian Sea.
基于 2011-2020 年 5 月卫星观测和再分析数据的挪威海中尺度锋面带分析
本研究的目的是比较根据卫星观测数据和再分析数据计算出的中尺度锋面带表面表现区域的水平温度梯度,既包括整个挪威海,也包括2011年至2020年5月中上层鱼类产卵洄游开始期间。 利用 MODIS/Aqua、GHRSST OSTIA 和 CMEMS GLORYS12v1 的月平均气温数据,得出了挪威海海面的月度和十年水平梯度场。对十年温度梯度估计值及其平均气候值进行了比较。大部分数据显示了挪威海主要锋面带的表面表现。根据独特的现场观测结果,对冰岛-法罗群岛锋面带地区的温度场进行了验证。结果表明,在分析挪威海的锋面带时,使用全球海温、盐度和温度观测系统 OSTIA 的温度场最为可取。所获得的中尺度锋面带的物理地理特征可用于评估它们与挪威海中上层鱼类洄游的关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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