Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets
CO2 is the strongest anthropogenic forcing agent for climate change since pre-industrial 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 emissio...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.150018 2023-05-15T13:45:35+02:00 Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets Dutton, Ellsworth G Michalsky, Joseph Schmithüsen, Holger Notholt, Justus König-Langlo, Gert Lemke, Peter Jung, Thomas LATITUDE: -89.983000 * LONGITUDE: -24.799000 * DATE/TIME START: 1994-01-01T00:00:00 * DATE/TIME END: 2012-12-31T23:59:00 2015-11-10 226 datasets https://doi.pangaea.de/10.1594/PANGAEA.150018 https://doi.org/10.1594/PANGAEA.150018 en eng PANGAEA Schmithüsen, Holger; Notholt, Justus; König-Langlo, Gert; Lemke, Peter; Jung, Thomas (2015): How increasing CO2 leads to an increased negative greenhouse effect in Antarctica. Geophysical Research Letters, 42(23), 10422-10428, https://doi.org/10.1002/2015GL066749 König-Langlo, Gert; Bücker, Amelie; Richter, Friedrich; Sieger, Rainer (2013): BSRN snapshot 2013-07 in two ISO image files (4.84 GB). PANGAEA, https://doi.org/10.1594/PANGAEA.833427 https://doi.pangaea.de/10.1594/PANGAEA.150018 https://doi.org/10.1594/PANGAEA.150018 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Antarctica Baseline Surface Radiation Network BSRN Monitoring station MONS South Pole SPO Dataset 2015 ftpangaea https://doi.org/10.1594/PANGAEA.150018 https://doi.org/10.1002/2015GL066749 https://doi.org/10.1594/PANGAEA.833427 2023-01-20T07:49:46Z CO2 is the strongest anthropogenic forcing agent for climate change since pre-industrial 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. Dataset Antarc* Antarctica South pole South pole PANGAEA - Data Publisher for Earth & Environmental Science South Pole ENVELOPE(-24.799000,-24.799000,-89.983000,-89.983000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Antarctica Baseline Surface Radiation Network BSRN Monitoring station MONS South Pole SPO |
spellingShingle |
Antarctica Baseline Surface Radiation Network BSRN Monitoring station MONS South Pole SPO Dutton, Ellsworth G Michalsky, Joseph Schmithüsen, Holger Notholt, Justus König-Langlo, Gert Lemke, Peter Jung, Thomas Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets |
topic_facet |
Antarctica Baseline Surface Radiation Network BSRN Monitoring station MONS South Pole SPO |
description |
CO2 is the strongest anthropogenic forcing agent for climate change since pre-industrial 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. |
format |
Dataset |
author |
Dutton, Ellsworth G Michalsky, Joseph Schmithüsen, Holger Notholt, Justus König-Langlo, Gert Lemke, Peter Jung, Thomas |
author_facet |
Dutton, Ellsworth G Michalsky, Joseph Schmithüsen, Holger Notholt, Justus König-Langlo, Gert Lemke, Peter Jung, Thomas |
author_sort |
Dutton, Ellsworth G |
title |
Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets |
title_short |
Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets |
title_full |
Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets |
title_fullStr |
Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets |
title_full_unstemmed |
Basic and other measurements of radiation from the Baseline Surface Radiation Network (BSRN) station South Pole (SPO) in the years 1994 to 2012, reference list of 226 datasets |
title_sort |
basic and other measurements of radiation from the baseline surface radiation network (bsrn) station south pole (spo) in the years 1994 to 2012, reference list of 226 datasets |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.150018 https://doi.org/10.1594/PANGAEA.150018 |
op_coverage |
LATITUDE: -89.983000 * LONGITUDE: -24.799000 * DATE/TIME START: 1994-01-01T00:00:00 * DATE/TIME END: 2012-12-31T23:59:00 |
long_lat |
ENVELOPE(-24.799000,-24.799000,-89.983000,-89.983000) |
geographic |
South Pole |
geographic_facet |
South Pole |
genre |
Antarc* Antarctica South pole South pole |
genre_facet |
Antarc* Antarctica South pole South pole |
op_relation |
Schmithüsen, Holger; Notholt, Justus; König-Langlo, Gert; Lemke, Peter; Jung, Thomas (2015): How increasing CO2 leads to an increased negative greenhouse effect in Antarctica. Geophysical Research Letters, 42(23), 10422-10428, https://doi.org/10.1002/2015GL066749 König-Langlo, Gert; Bücker, Amelie; Richter, Friedrich; Sieger, Rainer (2013): BSRN snapshot 2013-07 in two ISO image files (4.84 GB). PANGAEA, https://doi.org/10.1594/PANGAEA.833427 https://doi.pangaea.de/10.1594/PANGAEA.150018 https://doi.org/10.1594/PANGAEA.150018 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.150018 https://doi.org/10.1002/2015GL066749 https://doi.org/10.1594/PANGAEA.833427 |
_version_ |
1766227745443938304 |