Ice age temperatures and geochemistry

• Published in: Science
• Main Author: Bard, Edouard
• Other Authors: Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 1999
• Subjects: Other Topics; LAST GLACIAL MAXIMUM; NORTH-ATLANTIC; ICEBERG DISCHARGES; HEINRICH EVENTS; CLIMATE; CIRCULATION; OCEAN; GROUNDWATER; TRANSITIONS; RECORDS; Multidisciplinary Sciences; Science & Technology; 0036-8075; [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology; [SDE.MCG]Environmental Sciences/Global Changes; North Atlantic
• Online Access: https://hal.science/hal-00803098; https://doi.org/10.1126/science.284.5417.1133

Whether the last ice age was unusually chilly is more than merely historical curiosity. Such information is used to bench mark the computer models that are used to estimate future greenhouse warming. In his Perspective, Bard discusses recent efforts to use geochemical data to calculate past climate behavior. Data from noble gases in groundwater and trace elements in corals, for example, can indicate past sea surface temperatures. This can be compared with general circulation models, a comparison that shows good progress in modeling and also highlights where improvements can be made. According to the author, these advances have been made possible by the extensive exchanges of information between the data measurement and the modeling communities.