[{"language":[{"iso":"eng"}],"issue":"2","quality_controlled":"1","doi":"10.1029/2023JD040214","publication_identifier":{"issn":["2169-897X"],"eissn":["2169-8996"]},"scopus_import":"1","article_processing_charge":"Yes (in subscription journal)","article_type":"original","tmp":{"legal_code_url":"https://creativecommons.org/licenses/by/4.0/legalcode","image":"/images/cc_by.png","name":"Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)","short":"CC BY (4.0)"},"publication":"Journal of Geophysical Research: Atmospheres","department":[{"_id":"FrPe"}],"publisher":"Wiley","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","title":"Local controls on near-surface glacier cooling under warm atmospheric conditions","article_number":"e2023JD040214","file":[{"success":1,"file_name":"2024_JGRAtmospheres_Shaw.pdf","creator":"dernst","relation":"main_file","content_type":"application/pdf","file_size":7481087,"checksum":"cad5b93caadb40c14e5faedc34f7bba7","date_updated":"2024-02-06T08:38:27Z","file_id":"14943","access_level":"open_access","date_created":"2024-02-06T08:38:27Z"}],"day":"28","author":[{"orcid":"0000-0001-7640-6152","id":"3caa3f91-1f03-11ee-96ce-e0e553054d6e","full_name":"Shaw, Thomas","last_name":"Shaw","first_name":"Thomas"},{"first_name":"Pascal","last_name":"Buri","full_name":"Buri, Pascal","id":"317987aa-9421-11ee-ac5a-b941b041abba"},{"last_name":"Mccarthy","first_name":"Michael","full_name":"Mccarthy, Michael","id":"22a2674a-61ce-11ee-94b5-d18813baf16f"},{"full_name":"Miles, Evan S.","last_name":"Miles","first_name":"Evan S."},{"first_name":"Francesca","last_name":"Pellicciotti","orcid":"0000-0002-5554-8087","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","full_name":"Pellicciotti, Francesca"}],"citation":{"short":"T. Shaw, P. Buri, M. McCarthy, E.S. Miles, F. Pellicciotti, Journal of Geophysical Research: Atmospheres 129 (2024).","chicago":"Shaw, Thomas, Pascal Buri, Michael McCarthy, Evan S. Miles, and Francesca Pellicciotti. “Local Controls on Near-Surface Glacier Cooling under Warm Atmospheric Conditions.” <i>Journal of Geophysical Research: Atmospheres</i>. Wiley, 2024. <a href=\"https://doi.org/10.1029/2023JD040214\">https://doi.org/10.1029/2023JD040214</a>.","ieee":"T. Shaw, P. Buri, M. McCarthy, E. S. Miles, and F. Pellicciotti, “Local controls on near-surface glacier cooling under warm atmospheric conditions,” <i>Journal of Geophysical Research: Atmospheres</i>, vol. 129, no. 2. Wiley, 2024.","apa":"Shaw, T., Buri, P., McCarthy, M., Miles, E. S., &#38; Pellicciotti, F. (2024). Local controls on near-surface glacier cooling under warm atmospheric conditions. <i>Journal of Geophysical Research: Atmospheres</i>. Wiley. <a href=\"https://doi.org/10.1029/2023JD040214\">https://doi.org/10.1029/2023JD040214</a>","mla":"Shaw, Thomas, et al. “Local Controls on Near-Surface Glacier Cooling under Warm Atmospheric Conditions.” <i>Journal of Geophysical Research: Atmospheres</i>, vol. 129, no. 2, e2023JD040214, Wiley, 2024, doi:<a href=\"https://doi.org/10.1029/2023JD040214\">10.1029/2023JD040214</a>.","ista":"Shaw T, Buri P, McCarthy M, Miles ES, Pellicciotti F. 2024. Local controls on near-surface glacier cooling under warm atmospheric conditions. Journal of Geophysical Research: Atmospheres. 129(2), e2023JD040214.","ama":"Shaw T, Buri P, McCarthy M, Miles ES, Pellicciotti F. Local controls on near-surface glacier cooling under warm atmospheric conditions. <i>Journal of Geophysical Research: Atmospheres</i>. 2024;129(2). doi:<a href=\"https://doi.org/10.1029/2023JD040214\">10.1029/2023JD040214</a>"},"intvolume":"       129","related_material":{"record":[{"id":"14919","status":"public","relation":"research_data"}]},"status":"public","date_published":"2024-01-28T00:00:00Z","ddc":["550"],"has_accepted_license":"1","publication_status":"published","oa":1,"_id":"14885","year":"2024","acknowledgement":"This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No. 101026058. The authors acknowledge the invaluable field assistance of Marta Corrà, Achille Jouberton, Marin Kneib, Stefan Fugger, Celine Ducret and Alexander Groos. The authors would also like to thank Luca Carturan for advice regarding AWS setup and maintenance and Simone Fatichi for provision and support in the use of the Tethys-Chloris model. Open access funding provided by ETH-Bereich Forschungsanstalten.","date_created":"2024-01-28T23:01:42Z","file_date_updated":"2024-02-06T08:38:27Z","volume":129,"date_updated":"2024-02-06T08:44:02Z","abstract":[{"text":"The near-surface boundary layer can mediate the response of mountain glaciers to external climate, cooling the overlying air and promoting a density-driven glacier wind. The fundamental processes are conceptually well understood, though the magnitudes of cooling and presence of glacier winds are poorly quantified in space and time, increasing the forcing uncertainty for melt models. We utilize a new data set of on-glacier meteorological measurements on three neighboring glaciers in the Swiss Alps to explore their distinct response to regional climate under the extreme 2022 summer. We find that synoptic wind origins and local terrain modifications, not only glacier size, play an important role in the ability of a glacier to cool the near-surface air. Warm air intrusions from valley or synoptically-driven winds onto the glacier can occur between ∼19% and 64% of the time and contribute between 3% and 81% of the total sensible heat flux to the surface during warm afternoon hours, depending on the fetch of the glacier flowline and its susceptibility to boundary layer erosion. In the context of extreme summer warmth, indicative of future conditions, the boundary layer cooling (up to 6.5°C cooler than its surroundings) and resultant katabatic wind flow are highly heterogeneous between the study glaciers, highlighting the complex and likely non-linear response of glaciers to an uncertain future.","lang":"eng"}],"oa_version":"Published Version","month":"01","type":"journal_article"},{"quality_controlled":"1","doi":"10.1088/1748-9326/ad25a0","publication_identifier":{"issn":["1748-9326"]},"language":[{"iso":"eng"}],"keyword":["Public Health","Environmental and Occupational Health","General Environmental Science","Renewable Energy","Sustainability and the Environment"],"title":"Hydrological regimes and evaporative flux partitioning at the climatic ends of High Mountain Asia","day":"02","author":[{"last_name":"Fugger","first_name":"Stefan","full_name":"Fugger, Stefan","id":"86698d64-c4c6-11ee-af02-cdf1e6a7d31f"},{"id":"3caa3f91-1f03-11ee-96ce-e0e553054d6e","orcid":"0000-0001-7640-6152","full_name":"Shaw, Thomas","last_name":"Shaw","first_name":"Thomas"},{"full_name":"Jouberton, Achille","first_name":"Achille","last_name":"Jouberton"},{"first_name":"Evan","last_name":"Miles","full_name":"Miles, Evan"},{"id":"317987aa-9421-11ee-ac5a-b941b041abba","full_name":"Buri, Pascal","last_name":"Buri","first_name":"Pascal"},{"last_name":"McCarthy","first_name":"Michael","full_name":"McCarthy, Michael","id":"22a2674a-61ce-11ee-94b5-d18813baf16f"},{"first_name":"Catriona Louise","last_name":"Fyffe","id":"001b0422-8d15-11ed-bc51-cab6c037a228","full_name":"Fyffe, Catriona Louise"},{"full_name":"Fatichi, Simone","first_name":"Simone","last_name":"Fatichi"},{"full_name":"Kneib, Marin","first_name":"Marin","last_name":"Kneib"},{"first_name":"Peter","last_name":"Molnar","full_name":"Molnar, Peter"},{"full_name":"Pellicciotti, Francesca","orcid":"0000-0002-5554-8087","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","first_name":"Francesca","last_name":"Pellicciotti"}],"article_type":"original","tmp":{"legal_code_url":"https://creativecommons.org/licenses/by/4.0/legalcode","image":"/images/cc_by.png","name":"Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)","short":"CC BY (4.0)"},"article_processing_charge":"Yes","publication":"Environmental Research Letters","department":[{"_id":"FrPe"}],"user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","publisher":"IOP Publishing","main_file_link":[{"url":"https://doi.org/10.1088/1748-9326/ad25a0","open_access":"1"}],"ddc":["550"],"date_published":"2024-02-02T00:00:00Z","has_accepted_license":"1","publication_status":"accepted","oa":1,"citation":{"ama":"Fugger S, Shaw T, Jouberton A, et al. Hydrological regimes and evaporative flux partitioning at the climatic ends of High Mountain Asia. <i>Environmental Research Letters</i>. doi:<a href=\"https://doi.org/10.1088/1748-9326/ad25a0\">10.1088/1748-9326/ad25a0</a>","apa":"Fugger, S., Shaw, T., Jouberton, A., Miles, E., Buri, P., McCarthy, M., … Pellicciotti, F. (n.d.). Hydrological regimes and evaporative flux partitioning at the climatic ends of High Mountain Asia. <i>Environmental Research Letters</i>. IOP Publishing. <a href=\"https://doi.org/10.1088/1748-9326/ad25a0\">https://doi.org/10.1088/1748-9326/ad25a0</a>","ista":"Fugger S, Shaw T, Jouberton A, Miles E, Buri P, McCarthy M, Fyffe CL, Fatichi S, Kneib M, Molnar P, Pellicciotti F. Hydrological regimes and evaporative flux partitioning at the climatic ends of High Mountain Asia. Environmental Research Letters.","mla":"Fugger, Stefan, et al. “Hydrological Regimes and Evaporative Flux Partitioning at the Climatic Ends of High Mountain Asia.” <i>Environmental Research Letters</i>, IOP Publishing, doi:<a href=\"https://doi.org/10.1088/1748-9326/ad25a0\">10.1088/1748-9326/ad25a0</a>.","chicago":"Fugger, Stefan, Thomas Shaw, Achille Jouberton, Evan Miles, Pascal Buri, Michael McCarthy, Catriona Louise Fyffe, et al. “Hydrological Regimes and Evaporative Flux Partitioning at the Climatic Ends of High Mountain Asia.” <i>Environmental Research Letters</i>. IOP Publishing, n.d. <a href=\"https://doi.org/10.1088/1748-9326/ad25a0\">https://doi.org/10.1088/1748-9326/ad25a0</a>.","ieee":"S. Fugger <i>et al.</i>, “Hydrological regimes and evaporative flux partitioning at the climatic ends of High Mountain Asia,” <i>Environmental Research Letters</i>. IOP Publishing.","short":"S. Fugger, T. Shaw, A. Jouberton, E. Miles, P. Buri, M. McCarthy, C.L. Fyffe, S. Fatichi, M. Kneib, P. Molnar, F. Pellicciotti, Environmental Research Letters (n.d.)."},"status":"public","date_created":"2024-02-05T09:01:11Z","oa_version":"Published Version","type":"journal_article","month":"02","abstract":[{"text":"High elevation headwater catchments are complex hydrological systems that seasonally buffer water and release it in the form of snow and ice melt, modulating downstream runoff regimes and water availability. In High Mountain Asia (HMA), where a wide range of climates from semi-arid to monsoonal exist, the importance of the cryospheric contributions to the water budget varies with the amount and seasonal distribution of precipitation. Losses due to evapotranspiration and sublimation are to date largely unquantified components of the water budget in such catchments, although they can be comparable in magnitude to glacier melt contributions to streamflow. &amp;#xD;Here, we simulate the hydrology of three high elevation headwater catchments in distinct climates in HMA over 10 years using an ecohydrological model geared towards high-mountain areas including snow and glaciers, forced with reanalysis data. &amp;#xD;Our results show that evapotranspiration and sublimation together are most important at the semi-arid site, Kyzylsu, on the northernmost slopes of the Pamir mountain range. Here, the evaporative loss amounts to 28% of the water throughput, which we define as the total water added to, or removed from the water balance within a year. In comparison, evaporative losses are 19% at the Central Himalayan site Langtang and 13% at the wettest site, 24K, on the Southeastern Tibetan Plateau. At the three sites, respectively, sublimation removes 15%, 13% and 6% of snowfall, while evapotranspiration removes the equivalent of 76%, 28% and 19% of rainfall. In absolute terms, and across a comparable elevation range, the highest ET flux is 413 mm yr-1 at 24K, while the highest sublimation flux is 91 mm yr-1 at Kyzylsu. During warm and dry years, glacier melt was found to only partially compensate for the annual supply deficit.","lang":"eng"}],"date_updated":"2024-02-06T08:35:39Z","_id":"14938","year":"2024"},{"title":"Land surface modeling in the Himalayas: On the importance of evaporative fluxes for the water balance of a high-elevation catchment","article_number":"e2022WR033841","day":"25","file":[{"file_size":5554901,"relation":"main_file","content_type":"application/pdf","creator":"dernst","file_name":"2023_WaterResourcesResearch_Buri.pdf","success":1,"date_created":"2023-11-07T08:10:44Z","access_level":"open_access","file_id":"14495","date_updated":"2023-11-07T08:10:44Z","checksum":"7ba9c87228dc09029b16bc800a0ef1a1"}],"author":[{"full_name":"Buri, Pascal","last_name":"Buri","first_name":"Pascal"},{"full_name":"Fatichi, Simone","last_name":"Fatichi","first_name":"Simone"},{"first_name":"Thomas","last_name":"Shaw","id":"3caa3f91-1f03-11ee-96ce-e0e553054d6e","full_name":"Shaw, Thomas"},{"full_name":"Miles, Evan S.","last_name":"Miles","first_name":"Evan S."},{"first_name":"Michael","last_name":"Mccarthy","id":"22a2674a-61ce-11ee-94b5-d18813baf16f","full_name":"Mccarthy, Michael"},{"last_name":"Fyffe","first_name":"Catriona Louise","id":"001b0422-8d15-11ed-bc51-cab6c037a228","full_name":"Fyffe, Catriona Louise"},{"last_name":"Fugger","first_name":"Stefan","full_name":"Fugger, Stefan"},{"full_name":"Ren, Shaoting","last_name":"Ren","first_name":"Shaoting"},{"full_name":"Kneib, Marin","first_name":"Marin","last_name":"Kneib"},{"last_name":"Jouberton","first_name":"Achille","full_name":"Jouberton, Achille"},{"full_name":"Steiner, Jakob","last_name":"Steiner","first_name":"Jakob"},{"full_name":"Fujita, Koji","first_name":"Koji","last_name":"Fujita"},{"full_name":"Pellicciotti, Francesca","orcid":"0000-0002-5554-8087","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","first_name":"Francesca","last_name":"Pellicciotti"}],"article_processing_charge":"Yes (via OA deal)","scopus_import":"1","article_type":"original","tmp":{"name":"Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)","short":"CC BY-NC-ND (4.0)","image":"/images/cc_by_nc_nd.png","legal_code_url":"https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode"},"publication":"Water Resources Research","department":[{"_id":"FrPe"}],"user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","publisher":"Wiley","quality_controlled":"1","doi":"10.1029/2022WR033841","publication_identifier":{"issn":["0043-1397"],"eissn":["1944-7973"]},"language":[{"iso":"eng"}],"issue":"10","file_date_updated":"2023-11-07T08:10:44Z","date_created":"2023-11-05T23:00:53Z","volume":59,"abstract":[{"lang":"eng","text":"High Mountain Asia (HMA) is among the most vulnerable water towers globally and yet future projections of water availability in and from its high-mountain catchments remain uncertain, as their hydrologic response to ongoing environmental changes is complex. Mechanistic modeling approaches incorporating cryospheric, hydrological, and vegetation processes in high spatial, temporal, and physical detail have never been applied for high-elevation catchments of HMA. We use a land surface model at high spatial and temporal resolution (100 m and hourly) to simulate the coupled dynamics of energy, water, and vegetation for the 350 km2 Langtang catchment (Nepal). We compare our model outputs for one hydrological year against a large set of observations to gain insight into the partitioning of the water balance at the subseasonal scale and across elevation bands. During the simulated hydrological year, we find that evapotranspiration is a key component of the total water balance, as it causes about the equivalent of 20% of all the available precipitation or 154% of the water production from glacier melt in the basin to return directly to the atmosphere. The depletion of the cryospheric water budget is dominated by snow melt, but at high elevations is primarily dictated by snow and ice sublimation. Snow sublimation is the dominant vapor flux (49%) at the catchment scale, accounting for the equivalent of 11% of snowfall, 17% of snowmelt, and 75% of ice melt, respectively. We conclude that simulations should consider sublimation and other evaporative fluxes explicitly, as otherwise water balance estimates can be ill-quantified."}],"date_updated":"2023-11-07T08:12:34Z","month":"10","oa_version":"Published Version","type":"journal_article","_id":"14487","year":"2023","acknowledgement":"This project has received funding from the JSPS-SNSF (Japan Society for the Promotion of Science and Swiss National Science Foundation) Bilateral Programmes project (HOPE, High-ele-vation precipitation in High Mountain Asia; Grant 183633), and the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (RAVEN, Rapid mass losses of debris-covered glaciers in High Mountain Asia; Grant 772751). We want to thank in particular T. Gurung, S. Joshi, J. Shea, W. Immerzeel, and others involved, as well as ICIMOD, for their efforts over the past years in observing the meteorology of the Langtang catchment, collecting and organizing the data and making them publicly available. We also thank the National Geographic Society (Grant NGS-61784R-19) and the Mount Everest Foundation (reference 19-24) for providing fieldwork funding for C. L. Fyffe. We thank T. Kramer for help with the WSL Hyperion cluster. We are grate-ful for comments by three anonymous reviewers and the Associate Editor, who greatly helped to improve the manuscript further. Open access funding provided by ETH-Bereich Forschungsanstalten.","ddc":["550"],"date_published":"2023-10-25T00:00:00Z","has_accepted_license":"1","oa":1,"publication_status":"published","citation":{"apa":"Buri, P., Fatichi, S., Shaw, T., Miles, E. S., McCarthy, M., Fyffe, C. L., … Pellicciotti, F. (2023). Land surface modeling in the Himalayas: On the importance of evaporative fluxes for the water balance of a high-elevation catchment. <i>Water Resources Research</i>. Wiley. <a href=\"https://doi.org/10.1029/2022WR033841\">https://doi.org/10.1029/2022WR033841</a>","ista":"Buri P, Fatichi S, Shaw T, Miles ES, McCarthy M, Fyffe CL, Fugger S, Ren S, Kneib M, Jouberton A, Steiner J, Fujita K, Pellicciotti F. 2023. Land surface modeling in the Himalayas: On the importance of evaporative fluxes for the water balance of a high-elevation catchment. Water Resources Research. 59(10), e2022WR033841.","mla":"Buri, Pascal, et al. “Land Surface Modeling in the Himalayas: On the Importance of Evaporative Fluxes for the Water Balance of a High-Elevation Catchment.” <i>Water Resources Research</i>, vol. 59, no. 10, e2022WR033841, Wiley, 2023, doi:<a href=\"https://doi.org/10.1029/2022WR033841\">10.1029/2022WR033841</a>.","ama":"Buri P, Fatichi S, Shaw T, et al. Land surface modeling in the Himalayas: On the importance of evaporative fluxes for the water balance of a high-elevation catchment. <i>Water Resources Research</i>. 2023;59(10). doi:<a href=\"https://doi.org/10.1029/2022WR033841\">10.1029/2022WR033841</a>","short":"P. Buri, S. Fatichi, T. Shaw, E.S. Miles, M. McCarthy, C.L. Fyffe, S. Fugger, S. Ren, M. Kneib, A. Jouberton, J. Steiner, K. Fujita, F. Pellicciotti, Water Resources Research 59 (2023).","chicago":"Buri, Pascal, Simone Fatichi, Thomas Shaw, Evan S. Miles, Michael McCarthy, Catriona Louise Fyffe, Stefan Fugger, et al. “Land Surface Modeling in the Himalayas: On the Importance of Evaporative Fluxes for the Water Balance of a High-Elevation Catchment.” <i>Water Resources Research</i>. Wiley, 2023. <a href=\"https://doi.org/10.1029/2022WR033841\">https://doi.org/10.1029/2022WR033841</a>.","ieee":"P. Buri <i>et al.</i>, “Land surface modeling in the Himalayas: On the importance of evaporative fluxes for the water balance of a high-elevation catchment,” <i>Water Resources Research</i>, vol. 59, no. 10. Wiley, 2023."},"intvolume":"        59","related_material":{"record":[{"relation":"research_data","status":"public","id":"14494"}]},"status":"public"},{"doi":"10.5281/ZENODO.8402426","date_published":"2023-10-03T00:00:00Z","ddc":["550"],"main_file_link":[{"url":"https://10.5281/ZENODO.8402426","open_access":"1"}],"oa":1,"has_accepted_license":"1","related_material":{"record":[{"id":"14487","status":"public","relation":"used_in_publication"}]},"citation":{"apa":"Buri, P., Fatichi, S., Shaw, T., Miles, E., McCarthy, M., Fyffe, C. L., … Pellicciotti, F. (2023). Model output data to “Land surface modeling in the Himalayas: on the importance of evaporative fluxes for the water balance of a high elevation catchment.” Zenodo. <a href=\"https://doi.org/10.5281/ZENODO.8402426\">https://doi.org/10.5281/ZENODO.8402426</a>","ista":"Buri P, Fatichi S, Shaw T, Miles E, McCarthy M, Fyffe CL, Fugger S, Ren S, Kneib M, Jouberton A, Steiner J, Fujita K, Pellicciotti F. 2023. Model output data to ‘Land surface modeling in the Himalayas: on the importance of evaporative fluxes for the water balance of a high elevation catchment’, Zenodo, <a href=\"https://doi.org/10.5281/ZENODO.8402426\">10.5281/ZENODO.8402426</a>.","mla":"Buri, Pascal, et al. <i>Model Output Data to “Land Surface Modeling in the Himalayas: On the Importance of Evaporative Fluxes for the Water Balance of a High Elevation Catchment.”</i> Zenodo, 2023, doi:<a href=\"https://doi.org/10.5281/ZENODO.8402426\">10.5281/ZENODO.8402426</a>.","ama":"Buri P, Fatichi S, Shaw T, et al. Model output data to “Land surface modeling in the Himalayas: on the importance of evaporative fluxes for the water balance of a high elevation catchment.” 2023. doi:<a href=\"https://doi.org/10.5281/ZENODO.8402426\">10.5281/ZENODO.8402426</a>","short":"P. Buri, S. Fatichi, T. Shaw, E. Miles, M. McCarthy, C.L. Fyffe, S. Fugger, S. Ren, M. Kneib, A. Jouberton, J. Steiner, K. Fujita, F. Pellicciotti, (2023).","chicago":"Buri, Pascal, Simone Fatichi, Thomas Shaw, Evan  Miles, Michael McCarthy, Catriona Louise Fyffe, Stefan Fugger, et al. “Model Output Data to ‘Land Surface Modeling in the Himalayas: On the Importance of Evaporative Fluxes for the Water Balance of a High Elevation Catchment.’” Zenodo, 2023. <a href=\"https://doi.org/10.5281/ZENODO.8402426\">https://doi.org/10.5281/ZENODO.8402426</a>.","ieee":"P. Buri <i>et al.</i>, “Model output data to ‘Land surface modeling in the Himalayas: on the importance of evaporative fluxes for the water balance of a high elevation catchment.’” Zenodo, 2023."},"status":"public","title":"Model output data to \"Land surface modeling in the Himalayas: on the importance of evaporative fluxes for the water balance of a high elevation catchment\"","date_created":"2023-11-07T08:01:39Z","author":[{"full_name":"Buri, Pascal","last_name":"Buri","first_name":"Pascal"},{"last_name":"Fatichi","first_name":"Simone","full_name":"Fatichi, Simone"},{"first_name":"Thomas","last_name":"Shaw","full_name":"Shaw, Thomas","id":"3caa3f91-1f03-11ee-96ce-e0e553054d6e"},{"last_name":"Miles","first_name":"Evan ","full_name":"Miles, Evan "},{"first_name":"Michael","last_name":"McCarthy","id":"22a2674a-61ce-11ee-94b5-d18813baf16f","full_name":"McCarthy, Michael"},{"full_name":"Fyffe, Catriona Louise","id":"001b0422-8d15-11ed-bc51-cab6c037a228","first_name":"Catriona Louise","last_name":"Fyffe"},{"full_name":"Fugger, Stefan","last_name":"Fugger","first_name":"Stefan"},{"full_name":"Ren, Shaoting","last_name":"Ren","first_name":"Shaoting"},{"full_name":"Kneib, Marin","first_name":"Marin","last_name":"Kneib"},{"full_name":"Jouberton, Achille","last_name":"Jouberton","first_name":"Achille"},{"last_name":"Steiner","first_name":"Jakob","full_name":"Steiner, Jakob"},{"first_name":"Koji","last_name":"Fujita","full_name":"Fujita, Koji"},{"full_name":"Pellicciotti, Francesca","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","orcid":"0000-0002-5554-8087","last_name":"Pellicciotti","first_name":"Francesca"}],"date_updated":"2023-11-07T08:12:35Z","day":"03","abstract":[{"text":"We provide i) gridded initial conditions (.tif), ii) modeled gridded monthly outputs (.tif), and iii) modeled hourly outputs at the station locations (.txt) for the hydrological year 2019. Information about the variables and units can be found in the figures (.png) associated to each dataset. Details about the datasets can be found in the original publication by Buri and others (2023).\r\n\r\nBuri, P., Fatichi, S., Shaw, T. E., Miles, E. S., McCarthy, M. J., Fyffe, C. L., ... & Pellicciotti, F. (2023). Land Surface Modeling in the Himalayas: On the Importance of Evaporative Fluxes for the Water Balance of a High‐Elevation Catchment. Water Resources Research, 59(10), e2022WR033841. DOI: 10.1029/2022WR033841","lang":"eng"}],"month":"10","oa_version":"Published Version","type":"research_data_reference","_id":"14494","article_processing_charge":"No","tmp":{"name":"Creative Commons Public Domain Dedication (CC0 1.0)","short":"CC0 (1.0)","image":"/images/cc_0.png","legal_code_url":"https://creativecommons.org/publicdomain/zero/1.0/legalcode"},"publisher":"Zenodo","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","year":"2023","department":[{"_id":"FrPe"}]},{"language":[{"iso":"eng"}],"quality_controlled":"1","doi":"10.1038/s41561-023-01331-y","publication_identifier":{"issn":["1752-0894"],"eissn":["1752-0908"]},"article_type":"original","tmp":{"legal_code_url":"https://creativecommons.org/licenses/by/4.0/legalcode","image":"/images/cc_by.png","name":"Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)","short":"CC BY (4.0)"},"article_processing_charge":"Yes (in subscription journal)","scopus_import":"1","publication":"Nature Geoscience","department":[{"_id":"FrPe"}],"user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","publisher":"Springer Nature","title":"Local cooling and drying induced by Himalayan glaciers under global warming","day":"04","file":[{"relation":"main_file","content_type":"application/pdf","file_size":6072603,"creator":"dernst","success":1,"file_name":"2023_NatureGeoscience_Salerno.pdf","date_created":"2023-12-11T10:11:19Z","access_level":"open_access","date_updated":"2023-12-11T10:11:19Z","file_id":"14671","checksum":"d5ae0d17069eebc6f454c8608cf83e21"}],"author":[{"full_name":"Salerno, Franco","last_name":"Salerno","first_name":"Franco"},{"full_name":"Guyennon, Nicolas","first_name":"Nicolas","last_name":"Guyennon"},{"full_name":"Yang, Kun","first_name":"Kun","last_name":"Yang"},{"id":"3caa3f91-1f03-11ee-96ce-e0e553054d6e","orcid":"0000-0001-7640-6152","full_name":"Shaw, Thomas","first_name":"Thomas","last_name":"Shaw"},{"full_name":"Lin, Changgui","last_name":"Lin","first_name":"Changgui"},{"full_name":"Colombo, Nicola","first_name":"Nicola","last_name":"Colombo"},{"first_name":"Emanuele","last_name":"Romano","full_name":"Romano, Emanuele"},{"last_name":"Gruber","first_name":"Stephan","full_name":"Gruber, Stephan"},{"first_name":"Tobias","last_name":"Bolch","full_name":"Bolch, Tobias"},{"full_name":"Alessandri, Andrea","last_name":"Alessandri","first_name":"Andrea"},{"full_name":"Cristofanelli, Paolo","first_name":"Paolo","last_name":"Cristofanelli"},{"full_name":"Putero, Davide","first_name":"Davide","last_name":"Putero"},{"full_name":"Diolaiuti, Guglielmina","last_name":"Diolaiuti","first_name":"Guglielmina"},{"full_name":"Tartari, Gianni","last_name":"Tartari","first_name":"Gianni"},{"full_name":"Verza, Gianpietro","last_name":"Verza","first_name":"Gianpietro"},{"full_name":"Thakuri, Sudeep","first_name":"Sudeep","last_name":"Thakuri"},{"last_name":"Balsamo","first_name":"Gianpaolo","full_name":"Balsamo, Gianpaolo"},{"full_name":"Miles, Evan S.","first_name":"Evan S.","last_name":"Miles"},{"last_name":"Pellicciotti","first_name":"Francesca","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","orcid":"0000-0002-5554-8087","full_name":"Pellicciotti, Francesca"}],"citation":{"ista":"Salerno F, Guyennon N, Yang K, Shaw T, Lin C, Colombo N, Romano E, Gruber S, Bolch T, Alessandri A, Cristofanelli P, Putero D, Diolaiuti G, Tartari G, Verza G, Thakuri S, Balsamo G, Miles ES, Pellicciotti F. 2023. Local cooling and drying induced by Himalayan glaciers under global warming. Nature Geoscience. 16, 1120–1127.","mla":"Salerno, Franco, et al. “Local Cooling and Drying Induced by Himalayan Glaciers under Global Warming.” <i>Nature Geoscience</i>, vol. 16, Springer Nature, 2023, pp. 1120–27, doi:<a href=\"https://doi.org/10.1038/s41561-023-01331-y\">10.1038/s41561-023-01331-y</a>.","apa":"Salerno, F., Guyennon, N., Yang, K., Shaw, T., Lin, C., Colombo, N., … Pellicciotti, F. (2023). Local cooling and drying induced by Himalayan glaciers under global warming. <i>Nature Geoscience</i>. Springer Nature. <a href=\"https://doi.org/10.1038/s41561-023-01331-y\">https://doi.org/10.1038/s41561-023-01331-y</a>","ama":"Salerno F, Guyennon N, Yang K, et al. Local cooling and drying induced by Himalayan glaciers under global warming. <i>Nature Geoscience</i>. 2023;16:1120-1127. doi:<a href=\"https://doi.org/10.1038/s41561-023-01331-y\">10.1038/s41561-023-01331-y</a>","short":"F. Salerno, N. Guyennon, K. Yang, T. Shaw, C. Lin, N. Colombo, E. Romano, S. Gruber, T. Bolch, A. Alessandri, P. Cristofanelli, D. Putero, G. Diolaiuti, G. Tartari, G. Verza, S. Thakuri, G. Balsamo, E.S. Miles, F. Pellicciotti, Nature Geoscience 16 (2023) 1120–1127.","ieee":"F. Salerno <i>et al.</i>, “Local cooling and drying induced by Himalayan glaciers under global warming,” <i>Nature Geoscience</i>, vol. 16. Springer Nature, pp. 1120–1127, 2023.","chicago":"Salerno, Franco, Nicolas Guyennon, Kun Yang, Thomas Shaw, Changgui Lin, Nicola Colombo, Emanuele Romano, et al. “Local Cooling and Drying Induced by Himalayan Glaciers under Global Warming.” <i>Nature Geoscience</i>. Springer Nature, 2023. <a href=\"https://doi.org/10.1038/s41561-023-01331-y\">https://doi.org/10.1038/s41561-023-01331-y</a>."},"related_material":{"link":[{"relation":"press_release","url":"https://ista.ac.at/en/news/wind-of-climate-change/","description":"News on ISTA website"}]},"intvolume":"        16","status":"public","date_published":"2023-12-04T00:00:00Z","ddc":["550"],"has_accepted_license":"1","oa":1,"publication_status":"published","_id":"14659","year":"2023","acknowledgement":"This work was carried out within the framework of the EV-K2-CNR and Nepal Academy of Science and Technology. K.Y. was supported by the Second Tibetan Plateau Scientific Expedition and Research Program (grant no. 2019QZKK0206). N.C. was supported by the project NODES, which has received funding from the MUR–M4C2 1.5 of PNRR funded by the European Union - NextGeneration EU (Grant agreement no. ECS00000036). T.E.S. has received funding from the European Union’s Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant no. 101026058. F.P. has received funding from the European Research Council under the European Union’s Horizon 2020 research and innovation programme grant no. 772751, RAVEN, ‘Rapid mass losses of debris-covered glaciers in High Mountain Asia’ and has been supported by the SNSF grant ‘High-elevation precipitation in High Mountain Asia’ (grant no. 183633). A.A. was supported by the European Union’s Horizon 2020 research and innovation program under grant agreement no. 101004156 (CONFESS project) and by the European Union’s Horizon Europe research and innovation program under grant agreement no. 101081193 (OptimESM project). We thank H. Wehrli for valuable comments and suggestions and J. Giannitrapani for the graphic support. We thank A. Da Polenza and K. Bista of EV-K2-CNR for believing that studying the high elevations is relevant for the whole globe.","date_created":"2023-12-10T23:00:58Z","file_date_updated":"2023-12-11T10:11:19Z","volume":16,"type":"journal_article","oa_version":"Published Version","month":"12","abstract":[{"lang":"eng","text":"Understanding the response of Himalayan glaciers to global warming is vital because of their role as a water source for the Asian subcontinent. However, great uncertainties still exist on the climate drivers of past and present glacier changes across scales. Here, we analyse continuous hourly climate station data from a glacierized elevation (Pyramid station, Mount Everest) since 1994 together with other ground observations and climate reanalysis. We show that a decrease in maximum air temperature and precipitation occurred during the last three decades at Pyramid in response to global warming. Reanalysis data suggest a broader occurrence of this effect in the glacierized areas of the Himalaya. We hypothesize that the counterintuitive cooling is caused by enhanced sensible heat exchange and the associated increase in glacier katabatic wind, which draws cool air downward from higher elevations. The stronger katabatic winds have also lowered the elevation of local wind convergence, thereby diminishing precipitation in glacial areas and negatively affecting glacier mass balance. This local cooling may have partially preserved glaciers from melting and could help protect the periglacial environment."}],"date_updated":"2023-12-13T11:01:10Z","page":"1120-1127"},{"publisher":"Zenodo","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","department":[{"_id":"FrPe"}],"year":"2023","_id":"14919","article_processing_charge":"No","author":[{"id":"3caa3f91-1f03-11ee-96ce-e0e553054d6e","orcid":"0000-0001-7640-6152","full_name":"Shaw, Thomas","last_name":"Shaw","first_name":"Thomas"},{"id":"317987aa-9421-11ee-ac5a-b941b041abba","full_name":"Buri, Pascal","first_name":"Pascal","last_name":"Buri"},{"first_name":"Michael","last_name":"McCarthy","full_name":"McCarthy, Michael"},{"full_name":"Miles, Evan","first_name":"Evan","last_name":"Miles"},{"last_name":"Pellicciotti","first_name":"Francesca","full_name":"Pellicciotti, Francesca","orcid":"0000-0002-5554-8087","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70"}],"month":"08","oa_version":"Published Version","type":"research_data_reference","abstract":[{"text":"GLACIER METEOROLOGICAL DATA SWISS ALPS -2022\r\n","lang":"eng"}],"day":"23","date_updated":"2024-02-06T08:44:01Z","title":"Air temperature and near-surface meteorology datasets on three Swiss glaciers - Extreme 2022 Summer","date_created":"2024-01-31T12:08:26Z","status":"public","related_material":{"record":[{"id":"14885","status":"public","relation":"used_in_publication"}]},"citation":{"ama":"Shaw T, Buri P, McCarthy M, Miles E, Pellicciotti F. Air temperature and near-surface meteorology datasets on three Swiss glaciers - Extreme 2022 Summer. 2023. doi:<a href=\"https://doi.org/10.5281/ZENODO.8277285\">10.5281/ZENODO.8277285</a>","apa":"Shaw, T., Buri, P., McCarthy, M., Miles, E., &#38; Pellicciotti, F. (2023). Air temperature and near-surface meteorology datasets on three Swiss glaciers - Extreme 2022 Summer. Zenodo. <a href=\"https://doi.org/10.5281/ZENODO.8277285\">https://doi.org/10.5281/ZENODO.8277285</a>","mla":"Shaw, Thomas, et al. <i>Air Temperature and Near-Surface Meteorology Datasets on Three Swiss Glaciers - Extreme 2022 Summer</i>. Zenodo, 2023, doi:<a href=\"https://doi.org/10.5281/ZENODO.8277285\">10.5281/ZENODO.8277285</a>.","ista":"Shaw T, Buri P, McCarthy M, Miles E, Pellicciotti F. 2023. Air temperature and near-surface meteorology datasets on three Swiss glaciers - Extreme 2022 Summer, Zenodo, <a href=\"https://doi.org/10.5281/ZENODO.8277285\">10.5281/ZENODO.8277285</a>.","chicago":"Shaw, Thomas, Pascal Buri, Michael McCarthy, Evan Miles, and Francesca Pellicciotti. “Air Temperature and Near-Surface Meteorology Datasets on Three Swiss Glaciers - Extreme 2022 Summer.” Zenodo, 2023. <a href=\"https://doi.org/10.5281/ZENODO.8277285\">https://doi.org/10.5281/ZENODO.8277285</a>.","ieee":"T. Shaw, P. Buri, M. McCarthy, E. Miles, and F. Pellicciotti, “Air temperature and near-surface meteorology datasets on three Swiss glaciers - Extreme 2022 Summer.” Zenodo, 2023.","short":"T. Shaw, P. Buri, M. McCarthy, E. Miles, F. Pellicciotti, (2023)."},"oa":1,"date_published":"2023-08-23T00:00:00Z","doi":"10.5281/ZENODO.8277285","ddc":["550"],"main_file_link":[{"open_access":"1","url":"https://doi.org/10.5281/ZENODO.8277285"}]}]