In addition, from 2000 to 2015, there is an increasing trend in total water path, with the lowest value in 2005 at approximately 109 g/km 2 and the highest value in 2010 at around 130 g/km 2 (Fig. 4 ).
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Assessing spatiotemporal characteristics of atmospheric water cycle processes over the Tibetan Plateau using the WRF model and finer box model.
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