Results 101 to 110 of about 2,210 (216)
Land‐Atmosphere Coupling Contributing to Anomalous Rainfall Before the Onset of Australian Monsoon
Abstract This study applies idealized climate model simulations to investigate the influence of a continent‐sized ponded surface of limited heat capacity on the regional and remote atmospheric state. The analysis focuses on the wet season in northern Australia where precipitation provides critical water resources for agriculture and inland ecosystems ...
Z. Yang +5 more
wiley +1 more source
Decadal Reversal of Eurasian Winter Temperature Trend Linked to North Atlantic Climate Variability
Abstract The long‐term trend of Eurasian winter surface air temperature has undergone a distinct decadal change, shifting from a pronounced cooling trend between the late 1980s and late 2000s to a subsequent warming trend. This study demonstrates that this trend reversal is partly driven by decadal changes in North Atlantic sea surface temperature (SST)
Ye‐Jun Jun +5 more
wiley +1 more source
Using a reanalysis dataset and large‐ensemble simulation results, this study examines a possible factor of increasing trend in early winter precipitation in recent decades in the Hokuriku region of Japan.
Kazuto Takemura +2 more
doaj +1 more source
Wave Climate Trends and Teleconnections in the Gulf of Mexico and the Caribbean Sea
The Gulf of Mexico and the Caribbean Sea are key regions of the western Atlantic, where sea-state conditions are critical for coastal safety and offshore operations.
Miqueas Diaz-Maya +2 more
doaj +1 more source
Abstract Declining monsoon rainfall over agriculture‐dependent Eastern Central India (ECI) during 1901–2014 threatens regional food and water security. Observations link ECI drying to rapid Northwest Indian Ocean (NWIO) warming, which weakens monsoon circulation.
Yunfan Chen +7 more
wiley +1 more source
On the teleconnectivity of the “Arctic Oscillation”
The term “Arctic Oscillation” (AO) has recently been introduced to describe the leading structure of SLP variability over the Northern Hemisphere. A key feature of the AO is its zonally symmetric appearance, with a primary center of action over the Arctic and opposing anomalies in midlatitudes.
openaire +1 more source
The Impact of ENSO on Euro‐Atlantic Circulation a Year Later via Long‐Lived Tropical SST Anomalies
Abstract The second winter response to ENSO in the Euro‐Atlantic sector is a surprising recent discovery, however, the underlying mechanisms remain uncertain and are challenging to determine from observations. Here we revisit the second winter response to ENSO using multiple large ensemble climate model simulations to examine its robustness and ...
Christopher H. O’Reilly +2 more
wiley +1 more source
The Source of Arctic Precipitation in HadGEM3‐GC5
Abstract Snow and rain are increasing in the Arctic. Climate model projections indicate a 50% increase in precipitation by the end of the century. This increase is driven by increased local evaporation following reduced sea ice coverage alongside enhanced global evaporation and transport into the Arctic.
J. K. Ridley +3 more
wiley +1 more source
The El Niño–Southern Oscillation (ENSO) teleconnections over East Asia display inconsistency between early and late winter, yet the undering physical mechanisms remain unclear. Employing causal inference analysis, including Liang-Kleeman information flow
Xiadong An +3 more
doaj +1 more source
From teleconnection to telecoupling
published first as (erstmalig folgendermaßen erschienen): Cecilie Friis, Jonas Østergaard Nielsen, Iago Otero, Helmut Haberl, Jörg Niewöhner, and Patrick Hostert: “From teleconnection to telecoupling. Taking stock of an emerging framework in land system science”. In: Journal of Land Use Science 11.2 (2015), pages 131– 153.
Friis, Cecilie +5 more
openaire +1 more source

