How increasing CO2 leads to an increased negative greenhouse effect in Antarctica. Issue 23 (14th December 2015)

• Record Type: Journal Article
• Authors: Schmithüsen, Holger; Notholt, Justus; König‐Langlo, Gert; Lemke, Peter; Jung, Thomas
• Is Part Of: Geophysical research letters. Volume 42:Issue 23(2015:Dec.)
• Page Start: 10, 422
• Page End: 10, 428
• Publication Date: 2015-12-14
• Subjects: Antarctica -- atmosphere -- CO2 -- cooling; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2015GL066749
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: CO2 is the strongest anthropogenic forcing agent for climate change since preindustrial times. Like other greenhouse gases, CO2 absorbs terrestrial surface radiation and causes emission from the atmosphere to space. As the surface is generally warmer than the atmosphere, the total long‐wave emission to space is commonly less than the surface emission. However, this does not hold true for the high elevated areas of central Antarctica. For this region, the emission to space is higher than the surface emission; and the greenhouse effect of CO2 is around zero or even negative, which has not been discussed so far. We investigated this in detail and show that for central Antarctica an increase in CO2 concentration leads to an increased long‐wave energy loss to space, which cools the Earth‐atmosphere system. These findings for central Antarctica are in contrast to the general warming effect of increasing CO2 . Key Points: Negative greenhouse effect occurs only over central Antarctica on yearly average Rising CO2 can induce slightly negative instantaneous radiative forcing in central Antarctica