_id,doi,title
14851,10.1002/piuz.202301690,Die faszinierende Topologie rotierender Quanten
14938,10.1088/1748-9326/ad25a0,Hydrological regimes and evaporative flux partitioning at the climatic ends of High Mountain Asia
11447,10.1007/s11538-022-01029-z,Relation between the number of peaks and the number of reciprocal sign epistatic interactions
12573,10.1038/s43247-022-00588-2,Supraglacial debris thickness and supply rate in High-Mountain Asia
12575,10.1029/2022ef002852,Glacier contributions to river discharge during the current Chilean megadrought
12576,10.1088/1748-9326/ac9008,Multi-decadal monsoon characteristics and glacier response in High Mountain Asia
12580,10.1029/2021ef002619,Knowledge priorities on climate change and water in the Upper Indus Basin: A horizon scanning exercise to identify the Top 100 research questions in social and natural sciences
12582,10.1088/1748-9326/ac6966,Controls on the relative melt rates of debris-covered glacier surfaces
9128,10.1088/1748-9326/ab7130,"Response of precipitation extremes to warming: What have we learned from theory and idealized cloud-resolving simulations, and what remains to be learned?"
10794,10.3389/fenvs.2015.00042,Bayesian inference for stochastic individual-based models of ecological systems: a pest control simulation study
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
12647,10.1659/mrd-journal-d-11-00097.1,Glaciers as a proxy to quantify the spatial distribution of precipitation in the Hunza basin
9146,10.1088/1748-9326/5/2/025207,"How closely do changes in surface and column water vapor follow Clausius–Clapeyron scaling in climate change simulations?"