24
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: not found
      • Article: not found

      Summer heat waves over western Europe 1880–2003, their relationship to large-scale forcings and predictability

      Read this article at

      ScienceOpenPublisher
      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          Related collections

          Most cited references49

          • Record: found
          • Abstract: not found
          • Article: not found

          Classification, Seasonality and Persistence of Low-Frequency Atmospheric Circulation Patterns

            Bookmark
            • Record: found
            • Abstract: not found
            • Article: not found

            Uncertainty estimates in regional and global observed temperature changes: A new data set from 1850

              Bookmark
              • Record: found
              • Abstract: found
              • Article: not found

              Land-atmosphere coupling and climate change in Europe.

              Increasing greenhouse gas concentrations are expected to enhance the interannual variability of summer climate in Europe and other mid-latitude regions, potentially causing more frequent heatwaves. Climate models consistently predict an increase in the variability of summer temperatures in these areas, but the underlying mechanisms responsible for this increase remain uncertain. Here we explore these mechanisms using regional simulations of recent and future climatic conditions with and without land-atmosphere interactions. Our results indicate that the increase in summer temperature variability predicted in central and eastern Europe is mainly due to feedbacks between the land surface and the atmosphere. Furthermore, they suggest that land-atmosphere interactions increase climate variability in this region because climatic regimes in Europe shift northwards in response to increasing greenhouse gas concentrations, creating a new transitional climate zone with strong land-atmosphere coupling in central and eastern Europe. These findings emphasize the importance of soil-moisture-temperature feedbacks (in addition to soil-moisture-precipitation feedbacks) in influencing summer climate variability and the potential migration of climate zones with strong land-atmosphere coupling as a consequence of global warming. This highlights the crucial role of land-atmosphere interactions in future climate change.
                Bookmark

                Author and article information

                Journal
                Climate Dynamics
                Clim Dyn
                Springer Nature
                0930-7575
                1432-0894
                August 2007
                March 2007
                : 29
                : 2-3
                : 251-275
                Article
                10.1007/s00382-007-0233-1
                5169d806-37ef-4a09-a59f-f35789d62deb
                © 2007
                History

                Comments

                Comment on this article