_id,doi,title
14851,10.1002/piuz.202301690,Die faszinierende Topologie rotierender Quanten
14564,10.1029/2022ms003391,"A shallow‐deep unified stochastic mass flux cumulus parameterization in the single column community climate model"
14752,10.1029/2023av000880,"How moisture shapes low‐level radiative cooling in subsidence regimes"
14779,10.1029/2023gl103043,"The decaying near‐surface boundary layer of a retreating alpine glacier"
12573,10.1038/s43247-022-00588-2,Supraglacial debris thickness and supply rate in High-Mountain Asia
9151,10.1029/2020ms002256,"Distortions of the rain distribution with warming, with and without self‐aggregation"
12584,10.3390/rs13245122,Multi-source hydrological data products to monitor High Asian river basins and regional water security
12588,10.1029/2020gl092150,"Supraglacial ice cliffs can substantially increase the mass loss of debris‐covered glaciers"
9125,10.1029/2020ms002164,"Self‐aggregation of convective clouds with interactive sea surface temperature"
9126,10.1029/2020ms002106,"What controls the water vapor isotopic composition near the surface of tropical oceans? Results from an analytical model constrained by large‐eddy simulations"
12593,10.1038/s41561-020-0615-0,"The state of rock debris covering Earth’s glaciers"
12604,10.1029/2018gl079678,Surface pond energy absorption across four Himalayan Glaciers accounts for 1/8 of total catchment ice loss
12610,10.3389/feart.2017.00069,"Pond dynamics and supraglacial-englacial connectivity on debris-covered Lirung Glacier, Nepal"
12638,10.5194/hess-17-3661-2013,Comparison of climate change signals in CMIP3 and CMIP5 multi-model ensembles and implications for Central Asian glaciers
12640,10.1038/ngeo1896,Rising river flows throughout the twenty-first century in two Himalayan glacierized watersheds
9148,10.1029/2009gl039667,A model for the relationship between tropical precipitation and column water vapor
