机译:融化的高山冰川富含活性氮,丰富了高海拔湖泊
Climate Change Institute, University of Maine, Orono, Maine 04469;
rnDepartment of Zoology, Miami University, Oxford, Ohio 45056;
rnU.S. Geological Survey, Water Resources Discipline, Lakewood, Colorado 80225;
rnU.S. Geological Survey, Water Resources Discipline, Lakewood, Colorado 80225;
rnClimate Change Institute, University of Maine, Orono, Maine 04469;
rnClimate Change Institute, University of Maine, Orono, Maine 04469;
rnDepartment of Geosciences, University of Nebraska-Lincoln, Lincoln, Nebraska 68588;
rnDepartment of Zoology, Miami University, Oxford, Ohio 45056;
rnDepartment of Earth & Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada;
机译:使用日常气温阈值来评估雪融化的膨胀,并通过 T i> -Index模型来评估高山冰川的量:Forni Glacier(意大利)的案例研究
机译:冰川阻塞的湖水爆发期间高山冰川地表地震活动变化的观测
机译:EEM-PARAFAC揭示的亚高山湖泊中溶解有机物(DOM)的光化学反应性:对受气候变化影响的高山湖泊中异源DOM命运的见解
机译:在Hoodocene期间在冰川国家公园,蒙大拿州的高山湖沉积物中的碳信号
机译:高山冰川湖的过程网络,特别是絮凝作用
机译:清澈和冰川喂养的高山湖泊中浮游动物的分布和紫外线防护策略
机译:融化的高山冰川用活性氮富集高海拔湖泊