ISSN: 2157-7617

Journal des sciences de la Terre et du changement climatique

Accès libre

Notre groupe organise plus de 3 000 séries de conférences Événements chaque année aux États-Unis, en Europe et en Europe. Asie avec le soutien de 1 000 autres Sociétés scientifiques et publie plus de 700 Open Access Revues qui contiennent plus de 50 000 personnalités éminentes, des scientifiques réputés en tant que membres du comité de rédaction.

Les revues en libre accès gagnent plus de lecteurs et de citations
700 revues et 15 000 000 de lecteurs Chaque revue attire plus de 25 000 lecteurs

Indexé dans
  • Indice source CAS (CASSI)
  • Index Copernic
  • Google Scholar
  • Sherpa Roméo
  • Accès en ligne à la recherche en environnement (OARE)
  • Ouvrir la porte J
  • JournalSeek de génamique
  • JournalTOC
  • Annuaire des périodiques d'Ulrich
  • Accès à la recherche mondiale en ligne sur l'agriculture (AGORA)
  • Centre international pour l'agriculture et les biosciences (CABI)
  • Recherche de référence
  • Université Hamdard
  • EBSCO AZ
  • OCLC-WorldCat
  • Invocation de quête
  • Catalogue en ligne SWB
  • Publons
  • Euro Pub
  • ICMJE
Partager cette page

Abstrait

Impact of Ponds on Local Climate: A Remote Sensing and GIS Contribution Application to the Ponds of Brenne (France)

Nedjai R, Azaroual A, Chlif K, Bensaid A, Al-Sayah M and Ysbaa L

The influence of climate change on water bodies, particularly large ones, has been the subject of numerous studies that have demonstrated significant modifications or disturbances of the hydrological cycle (lower water volumes, higher temperatures and disruption of thermal stratification, increased direct evaporation), either by interpretation of sedimentary records or by direct measurements. However, at the scale of small limnic entities, these changes are barely noticeable and are only translated by a mere human reflection of increased freshness and densification of fog masses in limnic areas. The results of direct field measurements carried out in the Brenne study sites coupled to indirect methods for surface temperature estimation (remote sensing) converge to indicate either a rise of a several degrees (4-5°C) on and around the water bodies during winter periods or a decrease in summer. The magnitude of these thermal anomalies increases in areas characterized by a high density of ponds, giving these areas a distinct characteristic climatic context. The thermal envelopes change according to the seasons and the types of weather and may at times exceed 100 m to 200 m of extension around the water bodies giving rise to a particular climatic atmosphere. The proximity of the ponds in Brenne and their density give the area a climatic character translated by weather types very different from its surrounding and neighboring regions. Due to their effect the oceanic climate character is locally masked at times and during periods of high thermal contrast.