Hydrometeorology and Hydroclimate
International audience Meteorology is the main driving force of hydrology along time, from the instantaneous states and processes until the monthly, seasonal, yearly, and sometimes multiyear sequences. Meteorology drives and impacts much of the hydrological flows and storages, thus water balance ter...
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ftagrocampouest:oai:HAL:hal-01377888v1 2024-02-04T10:01:08+01:00 Hydrometeorology and Hydroclimate Cudennec, Christophe Gelfan, Alexander Ren, Liliang Slimani, Mohamed Sol Agro et hydrosystème Spatialisation (SAS) Institut National de la Recherche Agronomique (INRA)-AGROCAMPUS OUEST AGROCAMPUS OUEST Laboratoire STE Institut National de la Recherche Agronomique de Tunisie (INRAT) 2016 https://hal.science/hal-01377888 en eng HAL CCSD Hindawi Publishing Corporation hal-01377888 https://hal.science/hal-01377888 ISSN: 1687-9309 Advances in Meteorology https://hal.science/hal-01377888 Advances in Meteorology, 2016 [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2016 ftagrocampouest 2024-01-09T23:45:10Z International audience Meteorology is the main driving force of hydrology along time, from the instantaneous states and processes until the monthly, seasonal, yearly, and sometimes multiyear sequences. Meteorology drives and impacts much of the hydrological flows and storages, thus water balance terms as well as hazards, across a geometric and functional interface. This interface develops within a certain thickness, yet thin regarding the planetary radius and critical for water and other dynamics. This heterogeneous Critical Zone ranges from the bottom of groundwater reservoirs to the top of the tree canopy [1], including surface water liquid and frozen and gaseous flows and storages. Complex space-time effects develop in this critical zone such as orographic and oceanic influences on moisture-precipitation dynamics, hydrogeomorphological structure-function relationships, upstream-downstream integration, subsystems connectivities, variability interdependences, and scaling issues [2–6]. In some geographic settings, this critical zone is further complexified by extreme conditions of some of the properties, such as dryness or wetness, groundwater geometries and dynamics, cryospheric developments (snow, ice, and permafrost), soil and land covers, water uses, and concentration of water-driven chemicals. Article in Journal/Newspaper Ice permafrost Agrocampus Ouest: HAL |
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Open Polar |
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Agrocampus Ouest: HAL |
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language |
English |
topic |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
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[SDU.STU]Sciences of the Universe [physics]/Earth Sciences Cudennec, Christophe Gelfan, Alexander Ren, Liliang Slimani, Mohamed Hydrometeorology and Hydroclimate |
topic_facet |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience Meteorology is the main driving force of hydrology along time, from the instantaneous states and processes until the monthly, seasonal, yearly, and sometimes multiyear sequences. Meteorology drives and impacts much of the hydrological flows and storages, thus water balance terms as well as hazards, across a geometric and functional interface. This interface develops within a certain thickness, yet thin regarding the planetary radius and critical for water and other dynamics. This heterogeneous Critical Zone ranges from the bottom of groundwater reservoirs to the top of the tree canopy [1], including surface water liquid and frozen and gaseous flows and storages. Complex space-time effects develop in this critical zone such as orographic and oceanic influences on moisture-precipitation dynamics, hydrogeomorphological structure-function relationships, upstream-downstream integration, subsystems connectivities, variability interdependences, and scaling issues [2–6]. In some geographic settings, this critical zone is further complexified by extreme conditions of some of the properties, such as dryness or wetness, groundwater geometries and dynamics, cryospheric developments (snow, ice, and permafrost), soil and land covers, water uses, and concentration of water-driven chemicals. |
author2 |
Sol Agro et hydrosystème Spatialisation (SAS) Institut National de la Recherche Agronomique (INRA)-AGROCAMPUS OUEST AGROCAMPUS OUEST Laboratoire STE Institut National de la Recherche Agronomique de Tunisie (INRAT) |
format |
Article in Journal/Newspaper |
author |
Cudennec, Christophe Gelfan, Alexander Ren, Liliang Slimani, Mohamed |
author_facet |
Cudennec, Christophe Gelfan, Alexander Ren, Liliang Slimani, Mohamed |
author_sort |
Cudennec, Christophe |
title |
Hydrometeorology and Hydroclimate |
title_short |
Hydrometeorology and Hydroclimate |
title_full |
Hydrometeorology and Hydroclimate |
title_fullStr |
Hydrometeorology and Hydroclimate |
title_full_unstemmed |
Hydrometeorology and Hydroclimate |
title_sort |
hydrometeorology and hydroclimate |
publisher |
HAL CCSD |
publishDate |
2016 |
url |
https://hal.science/hal-01377888 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
ISSN: 1687-9309 Advances in Meteorology https://hal.science/hal-01377888 Advances in Meteorology, 2016 |
op_relation |
hal-01377888 https://hal.science/hal-01377888 |
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1789966825018097664 |