Estimate of the Globing Warming Caused by the Retreat of Polar Sea Ice
Alfred Laubereau, Hristo Iglev

TL;DR
This paper estimates that melting polar sea ice has contributed more to recent global warming than greenhouse gases, highlighting the significant impact of albedo change on Earth's temperature increase.
Contribution
It introduces a simple 1-dimensional model quantifying the impact of polar sea ice loss on global warming, emphasizing its larger role compared to greenhouse gases.
Findings
Sea ice loss contributed approximately 0.55°C to warming since 1955.
Greenhouse gases contributed about 0.26°C to warming from 1880 to 2015.
Temperature response to sea ice loss has a delay of about 20 years.
Abstract
The growing concentrations of the greenhouse gases CO2, CH4 and N2O (GHG) in the atmosphere are often considered as the dominant cause for the global warming during the past decades. The reported temperature data however do not display a simple correlation with the concentration changes since 1880 so that other reasons are to be considered to contribute notably. An important feature in this context is the shrinking of the polar ice caps observed in recent years. We have studied the direct effect of the loss of global sea ice since 1955 on the mean global temperature estimating the corresponding decrease of the terrestrial albedo. Using a simple 1-dimensional model the global warming of the surface is computed that is generated by the increase of GHG and the albedo change. A modest effect by the GHG of 0.08 K is calculated for the period 1880 to 1955 with a further increase by 0.18K for…
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Taxonomy
TopicsAtmospheric and Environmental Gas Dynamics · Arctic and Antarctic ice dynamics · Atmospheric chemistry and aerosols
