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The relationship of surface air temperature, heat balance at the surface, and radiative balance at the top of atmosphere over the Asian territory of Russia using reanalysis and remote-sensing data

机译:使用重新分析和遥感数据,俄罗斯亚洲领土上的地表气温,地表热平衡和大气层顶部的辐射平衡之间的关系

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摘要

In this study over the Asian territory of Russia (ATR) (45° N-80° N, 60° E-180° E) for the period of 1979-2010 the temporal variability of the surface air temperature field was investigated. There are several climatic factors which can influence temperature variability including radiative balance at the top of atmosphere (TOA), heat balance at the surface, total cloud cover, and large-scale atmospheric circulation in the Northern Hemisphere. The contribution of these factors to temperature variability is also investigated. It was found that during the past decade, over the ATR, the process of warming prevails mainly in the warm season, but in the cold season it is either not as marked or there is cooling instead. In the winter season there is a positive relationship between temperature anomalies and anomalies in cloudiness, effective radiation, and the Arctic Oscillation (AO) index. During the same period, a negative relationship between anomalies of temperature and anomalies of net radiation at the TOA, net shortwave radiation at the surface, and the Scandinavian (SCAND) index was observed. In the summer season, the relationship between temperature and cloudiness becomes negative and the relationship between temperature and atmospheric circulation indices decreases. For the period 2001-2010, radiative fluxes obtained from reanalysis data sets Japanese Reanalysis Data (JRA-25) and Modern Era-Retrospective Analysis for Research and Applications (MERRA) were compared to satellite remotely sensed data project Clouds and the Earth's Radiant Energy System (CERES). It was found that there is a good agreement between estimates of the net radiation at the TOA calculated using reanalysis data and satellite data: the difference is about 1.5 W m~2 and the correlation coefficient is more than 0.7. As for the comparison of radiative fluxes estimates at the surface for clear sky, there is less difference between MERRA and CERES. So, during the period 2001-2010 the relation between atmospheric circulation and surface air temperature variability increased in winter months. Obtained regression models allow us to describe from 27% to 82% of temperature variability in different months if we take into account both circulation and radiative factors.
机译:在这项针对俄罗斯亚洲地区(ATR)(45°N-80°N,60°E-180°E)的研究中,研究了1979-2010年期间地面空气温度场的时间变化。有几种可能影响温度变化的气候因素,包括大气层顶部的辐射平衡(TOA),地表热量平衡,总云量以及北半球的大规模大气环流。还研究了这些因素对温度变化的影响。人们发现,在过去的十年中,在整个ATR期间,变暖的过程主要发生在暖季,而在寒冷的季节,变暖的趋势不那么明显,或者出现了降温。在冬季,温度异常与多云,有效辐射和北极涛动(AO)指数之间存在正相关关系。在同一时期,温度异常与TOA的净辐射,表面的短波净辐射以及斯堪的纳维亚(SCAND)指数之间呈负相关。在夏季,温度与混浊之间的关系变为负,温度与大气环流指数之间的关系减小。在2001年至2010年期间,将从再分析数据集日本再分析数据(JRA-25)和现代时代研究与应用回顾研究(MERRA)获得的辐射通量与卫星遥感数据项目“云”和地球的辐射能系统进行了比较。 (CERES)。结果发现,利用再分析数据和卫星数据计算出的TOA处的净辐射估计值之间有很好的一致性:相差约1.5 W m〜2,相关系数大于0.7。至于晴朗天空表面辐射通量估计值的比较,MERRA和CERES之间的差异较小。因此,在2001-2010年期间,冬季的大气环流与地表气温变化之间的关系增加。如果同时考虑到循环和辐射因素,则获得的回归模型可以使我们描述不同月份温度变化的27%至82%。

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  • 来源
    《International journal of remote sensing》 |2014年第15期|5878-5898|共21页
  • 作者单位

    Laboratory of Physics of Climatic Systems, Institute of Monitoring of Climatic and Ecological Systems SB RAS, Tomsk, Russia;

    Laboratory of Physics of Climatic Systems, Institute of Monitoring of Climatic and Ecological Systems SB RAS, Tomsk, Russia;

    Laboratory of Physics of Climatic Systems, Institute of Monitoring of Climatic and Ecological Systems SB RAS, Tomsk, Russia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
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