首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Climatological characteristics of the tropopause parameters derived from GPS/CHAMP and GPS/SAC-C measurements
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Climatological characteristics of the tropopause parameters derived from GPS/CHAMP and GPS/SAC-C measurements

机译:从GPS / CHAMP和GPS / SAC-C测量得出的对流层顶参数的气候特征

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摘要

We have analyzed the tropopause parameters using the data retrieved from the GPS occultation experiment on board the CHAMP and SAC-C satellites. In the present study we have considered 3–4 years of data. Tropopause parameters such as temperature, height, pressure, and potential temperature have been separately studied for the tropical and other regions. Comparison of the temperature profiles (obtained near the equator) by the CHAMP and SAC-C satellites with the radiosonde measurements indicates very good agreement at altitudes below the tropopause. Deviations of 1–2 K are seen above the tropopause level. Analysis of the tropopause parameters separately done for the tropics (20°S–20°N) indicates annual variations. The tropopause temperature and pressure variations are strongly correlated, and they both anticorrelate with the tropopause height. Annual oscillation is evident in the variations of tropopause parameters. The sampled data indicate some interannual variations. We have found that there are some differences between the cold point tropopause (CPT) and lapse rate tropopause (LRT) methods of estimates. The global structure of the tropopause indicates clear differences between the tropics and high-latitude regions. Seasonal variation is evident in the parameters; however, they are more prominent in the polar regions. The paper confirms that the CHAMP and SAC-C measurements of the tropopause parameters are complementary as there is very little difference between the two measurements.
机译:我们使用CHAMP和SAC-C卫星上GPS掩星实验获得的数据分析了对流层顶参数。在本研究中,我们考虑了3-4年的数据。对热带和其他地区的河豚参数如温度,高度,压力和潜在温度进行了单独研究。 CHAMP和SAC-C卫星的温度曲线(在赤道附近获得)与探空仪的测量结果相比较,表明在对流层顶以下的高度有很好的一致性。在对流层顶水平以上可以看到1-2 K的偏差。对热带地区(20°S–20°N)分别进行的对流层顶参数分析表明,每年都有变化。对流层顶的温度和压力变化密切相关,并且都与对流层顶的高度反相关。对流层顶参数的变化表明年振荡。采样数据表明一些年际变化。我们发现,估计的冷点对流绝热(CPT)与流失率对流绝经(LRT)方法之间存在一些差异。对流层顶的整体结构表明热带和高纬度地区之间存在明显差异。参数的季节变化明显;但是,它们在极地地区更为突出。本文确认对流层顶参数的CHAMP和SAC-C测量值是互补的,因为这两个测量值之间几乎没有差异。

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