机译:青藏高原北部山区多年冻土区冬季径流减少
Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China;
Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China;
Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China;
Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China|Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;
Lappeenranta Univ Technol, Lab Green Chem, Sammonkatu 12, FI-50130 Mikkeli, Finland;
Hydrological regime; Permafrost degradation; Runoff; Climate change; Tibetan Plateau;
机译:青藏高原多年冻土区北缘不同植被类型下土壤酶活性的变化
机译:Permafrost崩溃将高山苔原转移到碳源,但在青藏高原北部的N 2 SUB> 2 O和CH 4释放
机译:用热量追踪法估算青藏高原北部多年冻土区地表水与地下水的相互作用。
机译:藏高原多年冻土区与季节性冷冻地区的表面能预算比较
机译:北部中东地区区域阶段的地震衰减