Recent ground thermo-hydrological changes in a Tibetan endorheic catchment and implications for lake level changes

• Main Authors: Martin, Léo, Westermann, Sebastian, Magni, Michele, Brun, Fanny, Fiddes, Joel, Lei, Yanbin, Kraaijenbrink, Philip, Mathys, Tamara, Langer, Moritz, Allen, Simon, Immerzeel, Walter
• Other Authors: Universiteit Utrecht, University of Oslo (UiO), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Institut Fédéral de Recherches sur la Forêt, la Neige et le Paysage (WSL), Institut Fédéral de Recherches Suisse, Chinese Academy of Sciences Beijing (CAS), University of Fribourg, Humboldt University Of Berlin, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Partenaires INRAE, Universität Zürich Zürich = University of Zurich (UZH), Department of Physical Geography Urecht
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2022
• Subjects: [SDU.STU]Sciences of the Universe [physics]/Earth Sciences; Rapid Lake; permafrost
• Online Access: https://hal.science/hal-03964351; https://hal.science/hal-03964351/document; https://hal.science/hal-03964351/file/hess-2022-241.pdf; https://doi.org/10.5194/hess-2022-241

International audience Abstract. Climate change modifies the water and energy fluxes between the atmosphere and the surface in mountainous regions. This is particularly true over the Qinghai-Tibet Plateau (QTP), a major headwater region of the world, which has shown substantial hydrological changes...