SCIENTIFIC BACKGROUND AND OBJECTIVES. As the highest plateau in the world, the Tibetan Plateau (TP) directly impacts its surrounding climate and environment through atmospheric and hydrological processes. Meanwhile, the TP climate changed significantly (such as rapid warming, moistening, solar dimming, and wind stilling) over the past 30 years , which further altered its environment (e.g., glacier retreat, lake expansion, and permafrost degradation, etc.) and brought environmental risks and disasters to the plateau's surrounding regions. The "third pole" was proposed as a geographic element to cover the TP and its adjacent mountains (Qiu 2008), and the "Third Pole Environment" (TPE) was then launched as an international program in 2009, with intension to pool international efforts to reveal and quantify the "water-ice-air-ecosystem-human" interactions in this region (Yao et al. 2012). Among the multisphere interactions on the TP, soil moisture (SM) plays a fundamental role in controlling land surface energy partition, adjusting surface runoff and soil drainage, regulating canopy transpiration and carbon AFFILIATIONS: yang, Qin, y. Chen, anD Tang-key laboratory of tibetan environment changes and land surface Processes, institute of tibetan Plateau research, chinese Academy of sciences, Beijing, china; Zhao, han, LaZhu, Ding, Wu, anD Lin-key laboratory of tibetan environment changes and land surface Processes, institute of tibetan Plateau research, chinese Academy of sciences, and university of chinese Academy of sciences, Beijing, china; Z. Chencollege of global change and earth system science, Beijing normal university, Beijing, china; Lv-state key laboratory of resources and environmental information system, institute of geographic sciences and natural resources research, chinese Academy of sciences, Beijing, china CORRESPONDING AUTHOR: kun Yang, institute of tibetan Plateau research, chinese Academy of sciences, Bldg. 3, courtyard 16, lincui rd., chaoyang district,