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首页> 外文期刊>International journal of remote sensing >Validation of ground-based microwave radiometer data and its application in verifying atmospheric stability over Mahbubnagar during 2011 monsoon and post-monsoon seasons
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Validation of ground-based microwave radiometer data and its application in verifying atmospheric stability over Mahbubnagar during 2011 monsoon and post-monsoon seasons

机译:地面微波辐射计数据的验证及其在验证2011年季风季节和季风后季节的Mahbubnagar大气稳定性中的应用

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摘要

Atmospheric instabilities, mainly convection, depend on temperature distribution and moisture availability. The development of convection can often lead to the formation of clouds and precipitation, release of latent heat, etc. The initiation or development of instabilities has to be studied in detail with high-resolution, ground-based instruments such as ground-based microwave radiometric measurements. In this study we evaluated ground-based microwave radiometer data (MWR)-retrieved temperature and relative humidity profiles and compared these to radiosonde observations. Analysis showed that MWR-measured temperature (specific humidity) has a warm (wet) bias below 3 km and cold (dry) bias above that altitude. Correlation of stability indices estimated from radiometer and radiosonde showed fairly good correlation, with a correlation coefficient greater than 0.5 with 95% significance. MWR was then utilized for the verification of atmospheric stability over Mahbubnagar (16 degrees 44' N, 77 degrees 59' E), India, during the second half of the monsoon and start of post-monsoon seasons. Radiometric observations showed strong day-to-day variation of atmospheric parameters as well as thermodynamic indices during the monsoon, which were weak during the post-monsoon season. The seasonal mean of thermodynamic indices and the associated seasonal difference showed that thunderstorm potential is higher during the post-monsoon season over the study site.
机译:大气不稳定性(主要是对流)取决于温度分布和水分供应。对流的发展通常会导致云的形成和降水,潜热的释放等。不稳定性的引发或发展必须用高分辨率的地面仪器(例如地面微波辐射测量仪)进行详细研究。测量。在这项研究中,我们评估了地面微波辐射计数据(MWR)检索到的温度和相对湿度曲线,并将其与探空仪的观测结果进行了比较。分析表明,MWR测得的温度(比湿)在3 km以下有一个热(湿)偏差,在该高度以上有冷(干)偏差。由辐射计和探空仪估算的稳定性指标的相关性显示出相当好的相关性,相关系数大于0.5,具有95%的显着性。然后,在季风的后半部和季风后季节的开始期间,利用MWR来验证印度Mahbubnagar(北纬16度44',东经77度59')的大气稳定性。辐射观测表明,季风期间大气参数和热力学指数的日变化很大,而季风后季节则较弱。热力学指数的季节平均值和相关的季节差异表明,研究地点的季风后季节雷暴潜力更高。

著录项

  • 来源
    《International journal of remote sensing 》 |2015年第12期| 2920-2933| 共14页
  • 作者单位

    Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India;

    Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India;

    Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India;

    Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India;

    Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India;

    Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India;

  • 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
  • 中图分类
  • 关键词

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