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Evidence of solar and tropical-ocean forcing of hydroclimate cycles in southeastern Australia for the past 6500 years
Evidence of solar and tropical‐ocean forcing of climate cycles has been found in numerous palaeoclimate records. Numerical modelling studies show physical mechanisms by which direct and indirect solar forcing may affect climate, while there is mounting evidence of solar forcing of tropical ocean‐atm...
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Published in: | Geophysical research letters 2010-05, Vol.37 (10), p.n/a |
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description | Evidence of solar and tropical‐ocean forcing of climate cycles has been found in numerous palaeoclimate records. Numerical modelling studies show physical mechanisms by which direct and indirect solar forcing may affect climate, while there is mounting evidence of solar forcing of tropical ocean‐atmosphere teleconnections. This study has developed a 6500 year record of dust deposition, a proxy for regional hydroclimate variability for the Snowy Mountains region of Australia. Spectral analysis of the record provides evidence of statistically significant cycles in dust deposition of 35–43 years, 62–73 years, 161 years and 2200 years. These correlate with variability in solar irradiance and the Pacific Decadal Oscillation (PDO). We present evidence to support physical links between variability in solar irradiance and change in the hydroclimate of southeast Australia and suggest that the effects of global warming and solar maxima on atmospheric circulation over extra‐tropical regions may exacerbate these impacts. |
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Res. Lett</addtitle><description>Evidence of solar and tropical‐ocean forcing of climate cycles has been found in numerous palaeoclimate records. Numerical modelling studies show physical mechanisms by which direct and indirect solar forcing may affect climate, while there is mounting evidence of solar forcing of tropical ocean‐atmosphere teleconnections. This study has developed a 6500 year record of dust deposition, a proxy for regional hydroclimate variability for the Snowy Mountains region of Australia. Spectral analysis of the record provides evidence of statistically significant cycles in dust deposition of 35–43 years, 62–73 years, 161 years and 2200 years. These correlate with variability in solar irradiance and the Pacific Decadal Oscillation (PDO). 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warming</topic><topic>Hydroclimate</topic><topic>Irradiance</topic><topic>Marine</topic><topic>Maxima</topic><topic>Mountains</topic><topic>Oscillations</topic><topic>Paleoclimate</topic><topic>Paleoclimate science</topic><topic>solar</topic><topic>Spectral analysis</topic><topic>Tropical environments</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>McGowan, Hamish A.</creatorcontrib><creatorcontrib>Marx, Samuel K.</creatorcontrib><creatorcontrib>Soderholm, Joshua</creatorcontrib><creatorcontrib>Denholm, John</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research 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subjects | Atmospheric circulation Atmospheric sciences Australia Climate Climate change Deposition Dust Earth Earth sciences Earth, ocean, space Exact sciences and technology General circulation models Geophysics Global warming Hydroclimate Irradiance Marine Maxima Mountains Oscillations Paleoclimate Paleoclimate science solar Spectral analysis Tropical environments |
title | Evidence of solar and tropical-ocean forcing of hydroclimate cycles in southeastern Australia for the past 6500 years |
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