Abstract

The water vapor budget (WVB) over the Tibetan Plateau (TP) is closely related to the large-scale atmospheric moisture transportation of the surrounding mainland and oceans, especially for the Indo-Pacific warm pool (IPWP). However, the procession linkage between the WVBs over the TP and its inner basins and IPWP has not been sufficiently elucidated. In this study, the relationship between the summer WVB over the TP and the IPWP was quantitatively investigated using reanalysis datasets and satellite-observed sea surface temperature (SST). The results show that: (1) the mean total summer vapor budget (WVBt) over the TP in the period of 1979–2018 was 72.5 × 106 kg s−1. Additionally, for the 13 basins within the TP, the summer WVB has decreased from southeast to northwest; the Yarlung Zangbo River Basin had the highest WVB (33.7%), followed by the Upper Yangtze River Basin, Ganges River Basin and Qiangtang Plateau. (2) For the past several decades, the WVBt over the TP has experienced an increasing trend (3.81 × 106 kg s−1 decade−1), although the southern boundary budget (WVBs) contributed the most and is most closely related with the WVBt, while the eastern boundary budget (WVBe) experienced a decreasing trend (4.21 × 106 kg s−1 decade−1) which was almost equal to the interdecadal variations of the WVBt. (3) For the IPWP, we defined a new warm pool index of surface latent heat flux (WPI-slhf), and found that an increasing WPI-slhf would cause an anticyclone anomaly in the equatorial western Indian Ocean (near 70° E), resulting in the increased advent of water vapor to the TP. (4) On the interdecadal scale, the correlation coefficients of the variation of the summer WVBt over the TP with the WPI-slhf and Indian Ocean Dipole (IOD) signal were 0.86 and 0.85, respectively (significant at the 0.05% level). Therefore, the warming and the increasing slhf of the IPWP would significantly contribute to the increasing WVB of the TP in recent decades.

Highlights

  • As the “roof of the world”, the Tibetan Plateau (TP) has high elevations, with the average elevation exceeding 4000 m [1,2]

  • In spring and winter (Figure 2a,c), the high-value areas of water of water vapor flux are located in the west and southeast of the plateau; the water vapor mainly vapor flux are located in the west and southeast of the plateau; the water vapor mainly can be can be attributed to the westerly belt in the middle and high latitudes and the Arabian Sea in the attributed to the westerly belt in the middle and high latitudes and the Arabian Sea in the northern northern Indian Ocean

  • In this study, based on the latest ERA5 reanalysis product and satellite-observed sea surface temperature (SST), we have studied the variability characteristics of summer water vapor budget (WVB) over the TP and its 13 basins with high-resolution boundaries and analyzed the effects of the water vapor transport of the TP on the precipitable water (PW) and precipitation

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Summary

Introduction

As the “roof of the world”, the Tibetan Plateau (TP) has high elevations, with the average elevation exceeding 4000 m [1,2]. During boreal summer (June–July–August, JJA), the water vapor of the TP is primarily transported over large distances, from the tropical Indian Ocean and the Western Pacific Ocean [15,16], which is the most significant region of the global interannual variability of sea surface temperature (SST). This region contains the world’s largest warm pool with the highest SST, known as the Under the influence of global warming, TP’s water vapor has undergone drastic changes in recent decades, which has significantly affected the TP’s precipitation, lake storage and river runoff [9,10,11,12,13,14].

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