CAJ | 학술논문

青藏高原对亚洲季风环流的形成有重要作用，同时作为“世界屋脊”拥有丰富的冰川、积雪、河流、湖泊和地下蓄水层。青藏高原特殊大地形动力和热力作用深刻地影响着亚洲与全球大气水分循环，也对全球气候与环境产生深远的影响。基于青藏高原在亚洲夏季风系统大气水分循环过程的重要地位，从青藏高原对全球大气水分循环重要作用的视角，综述了青藏高原大气水分循环过程中青藏高原局地热力对流、高原的“阶梯式”水汽流爬升“第二类条件不稳定（CISK）”物理模型、青藏高原视热源结构影响及多尺度水汽汇流通道、海洋ˉ青藏高原“水汽源ˉ汇”结构、青藏高原跨半球垂直环流圈水分循环结构、青藏高原大气水分循环综合模型等的相关研究进展，剖析了青藏高原大气水分循环综合模型的研究背景，探讨了青藏高原特殊大地形热力驱动机制及其云水效应，描述出与青藏高原热力驱动的亚洲区域和跨半球垂直环流圈水分循环结构，揭示了青藏高原热力强迫与海洋ˉ大气ˉ陆地水文过程特殊的相互反馈作用。青藏高原发源的亚洲河流水系是为人口众多的亚洲区域供给生活、农业和工业用水的重要水资源之一。因此，认识在全球变暖背景下青藏高原的水分循环及其对水资源变化影响至关重要，仍需深入地探讨青藏高原大气水分循环机制及其全球影响效应。
청장고원대아주계풍배류적형성유중요작용，동시작위“세계옥척”옹유봉부적빙천、적설、하류、호박화지하축수층。청장고원특수대지형동력화열력작용심각지영향착아주여전구대기수분순배，야대전구기후여배경산생심원적영향。기우청장고원재아주하계풍계통대기수분순배과정적중요지위，종청장고원대전구대기수분순배중요작용적시각，종술료청장고원대기수분순배과정중청장고원국지열력대류、고원적“계제식”수기류파승“제이류조건불은정（CISK）”물리모형、청장고원시열원결구영향급다척도수기회류통도、해양ˉ청장고원“수기원ˉ회”결구、청장고원과반구수직배류권수분순배결구、청장고원대기수분순배종합모형등적상관연구진전，부석료청장고원대기수분순배종합모형적연구배경，탐토료청장고원특수대지형열력구동궤제급기운수효응，묘술출여청장고원열력구동적아주구역화과반구수직배류권수분순배결구，게시료청장고원열력강박여해양ˉ대기ˉ륙지수문과정특수적상호반궤작용。청장고원발원적아주하류수계시위인구음다적아주구역공급생활、농업화공업용수적중요수자원지일。인차，인식재전구변난배경하청장고원적수분순배급기대수자원변화영향지관중요，잉수심입지탐토청장고원대기수분순배궤제급기전구영향효응。
The Tibetan Plateau plays an important role in the development of Asian monsoon circulations.The Tibetan Plateau itself contains the richest water resources in the forms of snowpacks,glaciers,lakes,rivers,and aquifers.The mechanical and thermal forcing of the unique Tibetan Plateauˉtopography provides a profound impact on Asian and global water cycles as well as climate and environment changes.In view of the specially important role of the Tibetan Plateau in building Asian summer monsoon system,regional and global water cycles,the advances in study of the atmospheric water cycle over the Tibetan Platˉ eau are reviewed with the emphases on the respects of (1)the local convection in the atmosphere over the Tibetan Plateau,(2) the mechanism of the twoˉladder"CISK"in the vapor uplift to the Tibetan Plateau,(3)the structures of apparent heat source over the Tibetan Plateau with the multiˉscale vapor busway,(4)the patterns of sourceˉreceptor of vapor from oceans to the plateau,(5)the crossˉhemispheric water cycle in the vertical atmospheric circulation and (6)a comprehensive understanding of the atmospheric water cycle over the Tibetan Plateau.In the recent research,a comprehensive pattern of the atmospheric water cycle over the Tibetan Plateau is revealed;the mechanism on the thermal forcing of large Tibetan Plateauˉtopography and its effect on cloudˉprecipitation are investigated;the Asian regional and crossˉhemispheric vapor transport structures in the vertical atmospheric circulation driven by the Tibetan Plateau forcing are characterized;and the feedback interaction between the Tibetˉ an Plateau`s thermal forcing and the hydrological process of oceanˉatmosphereˉland is explored.The Asian rivers originating from the Tibetan Plateau have been sustaining the life,agricultural and industrial water usage for the Asian regions with a large population,and therefore,it is vital to understand the atmospheric water cycle and its impact on the changes in the Tibetan Plateau water resource under background of the global warming.The atmospheric water cycle process over the TP with the global effect is needed to further studied.