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Study on thermal infrared remote sensing of Yarlung Zangbo River and Bangong Co-Nujiang River suture belt in Qinghai-Tibet Plateau

机译:青藏高原雅鲁藏布江和班公怒江缝合带的热红外遥感研究。

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摘要

The area change of heat abnormity is not in accordance with conclusions of former thermal infrared remote sensing studies of the Qinghai-Tibet Plateau, which were that the temperature of Yarlung Zangbo River suture belt of the southern Plateau is high and the northern temperature is low. The study result in this paper shows that the highest temperature is found in the Bangong Co-Nujiang River suture belt, the Yarlung Zangbo River suture belt temperature is the second highest, and the northern Tibet temperature is the lowest. The study demonstration area was the suture belt areas of the Yarlung Zangbo River and the Bangong Co-Nujiang River in the Qinghai-Tibet Plateau, where the land temperature of the Qinghai-Tibet Plateau and the bore temperature of field land surface were measured and the emissivity of land surface was calculated. In addition, the authors explore the mechanism of the relationship between thermal infrared remote sensing and constructing thermodynamics and reach four new conclusions about the thermodynamics of the Tibet Plateau.
机译:热异常的面积变化与青藏高原以前的热红外遥感研究结论不符,青藏高原南部的雅鲁藏布江缝合带温度高,北部温度低。本文的研究结果表明,班公河-怒江缝合带温度最高,雅鲁藏布江缝合带温度第二高,藏北温度最低。研究示范区是青藏高原雅鲁藏布江和班公怒江的缝合带,测量了青藏高原的地温和田间地表的钻孔温度。计算出地表的发射率。此外,作者探索了热红外遥感与构造热力学之间关系的机理,并得出了关于青藏高原热力学的四个新结论。

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