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Potential role of winter rainfall in explaining increased moisture in the Mediterranean and Middle East during periods of maximum orbitally-forced insolation seasonality
by
Chen, G.
, Liu, Z.
, Edwards, R. L.
, Kutzbach, J. E.
, Cheng, H.
in
Atmospheric models
/ Climate
/ Climate models
/ Climatology
/ Demographic aspects
/ Earth and Environmental Science
/ Earth Sciences
/ Earth, ocean, space
/ Environmental aspects
/ Exact sciences and technology
/ Geophysics/Geodesy
/ Marine and continental quaternary
/ Middle East
/ monsoon season
/ Monsoons
/ Northern Africa
/ Oceanography
/ Orbits
/ Paleoclimate science
/ Precipitation
/ rain
/ Rain and rainfall
/ Seasonal variations
/ simulation models
/ solar radiation
/ Studies
/ Summer
/ Surficial geology
/ Winter
2014
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Potential role of winter rainfall in explaining increased moisture in the Mediterranean and Middle East during periods of maximum orbitally-forced insolation seasonality
by
Chen, G.
, Liu, Z.
, Edwards, R. L.
, Kutzbach, J. E.
, Cheng, H.
in
Atmospheric models
/ Climate
/ Climate models
/ Climatology
/ Demographic aspects
/ Earth and Environmental Science
/ Earth Sciences
/ Earth, ocean, space
/ Environmental aspects
/ Exact sciences and technology
/ Geophysics/Geodesy
/ Marine and continental quaternary
/ Middle East
/ monsoon season
/ Monsoons
/ Northern Africa
/ Oceanography
/ Orbits
/ Paleoclimate science
/ Precipitation
/ rain
/ Rain and rainfall
/ Seasonal variations
/ simulation models
/ solar radiation
/ Studies
/ Summer
/ Surficial geology
/ Winter
2014
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Potential role of winter rainfall in explaining increased moisture in the Mediterranean and Middle East during periods of maximum orbitally-forced insolation seasonality
by
Chen, G.
, Liu, Z.
, Edwards, R. L.
, Kutzbach, J. E.
, Cheng, H.
in
Atmospheric models
/ Climate
/ Climate models
/ Climatology
/ Demographic aspects
/ Earth and Environmental Science
/ Earth Sciences
/ Earth, ocean, space
/ Environmental aspects
/ Exact sciences and technology
/ Geophysics/Geodesy
/ Marine and continental quaternary
/ Middle East
/ monsoon season
/ Monsoons
/ Northern Africa
/ Oceanography
/ Orbits
/ Paleoclimate science
/ Precipitation
/ rain
/ Rain and rainfall
/ Seasonal variations
/ simulation models
/ solar radiation
/ Studies
/ Summer
/ Surficial geology
/ Winter
2014
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Potential role of winter rainfall in explaining increased moisture in the Mediterranean and Middle East during periods of maximum orbitally-forced insolation seasonality
Journal Article
Potential role of winter rainfall in explaining increased moisture in the Mediterranean and Middle East during periods of maximum orbitally-forced insolation seasonality
2014
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Overview
Precession-related forcing of seasonal insolation changes in the northern hemisphere (NH) alternates between maximum NH seasonality (summer perihelion–increased insolation; winter aphelion–decreased insolation) and minimum NH seasonality (summer aphelion, and winter perihelion). With maximum NH seasonality, climate models simulate stronger NH summer monsoons that bring increased precipitation to North Africa and South and East Asia, in agreement with the in-phase relation of precipitation and NH summer insolation found in many paleoclimatic records. However paleoclimatic records in parts of the Mediterranean, the Middle East, and the interior of Asia also indicate increased moisture at times of maximum NH seasonality, a change not always clearly linked to stronger summer monsoons—either because these regions are at or beyond the boundaries of the present-day monsoon or because the observations allow multiple causal interpretations, or both. This study focuses on the possible role of changes in NH winter climate in explaining these wetter episodes. Using climate model simulations, we show that the ‘NH winter aphelion–decreased NH winter insolation’ orbital configuration is linked to the Mediterranean storm track and increased winter rains in the Mediterranean, the Middle East, and interior Asia. We conclude that wetter periods at precession time scales in these particular regions may have resulted either from increased wintertime storm track precipitation, or from a combination of increased winter and summer rainfall. Given this seasonal ambiguity, both possibilities need to be considered.
Publisher
Springer Berlin Heidelberg,Springer,Springer Nature B.V
Subject
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