Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback
Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of...
Ausführliche Beschreibung
Autor*in: |
Zhou, Tianjun [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
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2015 |
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Anmerkung: |
© The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 |
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Übergeordnetes Werk: |
Enthalten in: Acta Meteorologica Sinica - The Chinese Meteorological Society, 2011, 29(2015), 6 vom: Dez., Seite 884-895 |
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Übergeordnetes Werk: |
volume:29 ; year:2015 ; number:6 ; month:12 ; pages:884-895 |
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DOI / URN: |
10.1007/s13351-015-5036-4 |
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Katalog-ID: |
SPR031428118 |
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10.1007/s13351-015-5036-4 doi (DE-627)SPR031428118 (SPR)s13351-015-5036-4-e DE-627 ger DE-627 rakwb eng Zhou, Tianjun verfasserin aut Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. climate sensitivity (dpeaa)DE-He213 radiative forcing (dpeaa)DE-He213 climate feedback (dpeaa)DE-He213 2°C threshold (dpeaa)DE-He213 greenhouse gases (dpeaa)DE-He213 climate model (dpeaa)DE-He213 Chen, Xiaolong aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 29(2015), 6 vom: Dez., Seite 884-895 (DE-627)SPR031424376 nnns volume:29 year:2015 number:6 month:12 pages:884-895 https://dx.doi.org/10.1007/s13351-015-5036-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 29 2015 6 12 884-895 |
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10.1007/s13351-015-5036-4 doi (DE-627)SPR031428118 (SPR)s13351-015-5036-4-e DE-627 ger DE-627 rakwb eng Zhou, Tianjun verfasserin aut Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. climate sensitivity (dpeaa)DE-He213 radiative forcing (dpeaa)DE-He213 climate feedback (dpeaa)DE-He213 2°C threshold (dpeaa)DE-He213 greenhouse gases (dpeaa)DE-He213 climate model (dpeaa)DE-He213 Chen, Xiaolong aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 29(2015), 6 vom: Dez., Seite 884-895 (DE-627)SPR031424376 nnns volume:29 year:2015 number:6 month:12 pages:884-895 https://dx.doi.org/10.1007/s13351-015-5036-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 29 2015 6 12 884-895 |
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10.1007/s13351-015-5036-4 doi (DE-627)SPR031428118 (SPR)s13351-015-5036-4-e DE-627 ger DE-627 rakwb eng Zhou, Tianjun verfasserin aut Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. climate sensitivity (dpeaa)DE-He213 radiative forcing (dpeaa)DE-He213 climate feedback (dpeaa)DE-He213 2°C threshold (dpeaa)DE-He213 greenhouse gases (dpeaa)DE-He213 climate model (dpeaa)DE-He213 Chen, Xiaolong aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 29(2015), 6 vom: Dez., Seite 884-895 (DE-627)SPR031424376 nnns volume:29 year:2015 number:6 month:12 pages:884-895 https://dx.doi.org/10.1007/s13351-015-5036-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 29 2015 6 12 884-895 |
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10.1007/s13351-015-5036-4 doi (DE-627)SPR031428118 (SPR)s13351-015-5036-4-e DE-627 ger DE-627 rakwb eng Zhou, Tianjun verfasserin aut Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. climate sensitivity (dpeaa)DE-He213 radiative forcing (dpeaa)DE-He213 climate feedback (dpeaa)DE-He213 2°C threshold (dpeaa)DE-He213 greenhouse gases (dpeaa)DE-He213 climate model (dpeaa)DE-He213 Chen, Xiaolong aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 29(2015), 6 vom: Dez., Seite 884-895 (DE-627)SPR031424376 nnns volume:29 year:2015 number:6 month:12 pages:884-895 https://dx.doi.org/10.1007/s13351-015-5036-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 29 2015 6 12 884-895 |
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10.1007/s13351-015-5036-4 doi (DE-627)SPR031428118 (SPR)s13351-015-5036-4-e DE-627 ger DE-627 rakwb eng Zhou, Tianjun verfasserin aut Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. climate sensitivity (dpeaa)DE-He213 radiative forcing (dpeaa)DE-He213 climate feedback (dpeaa)DE-He213 2°C threshold (dpeaa)DE-He213 greenhouse gases (dpeaa)DE-He213 climate model (dpeaa)DE-He213 Chen, Xiaolong aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 29(2015), 6 vom: Dez., Seite 884-895 (DE-627)SPR031424376 nnns volume:29 year:2015 number:6 month:12 pages:884-895 https://dx.doi.org/10.1007/s13351-015-5036-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 29 2015 6 12 884-895 |
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Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 |
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Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 |
abstract_unstemmed |
Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. Challenges that call for further investigation in the research community, in particular the Chinese community, are discussed. © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 |
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Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR031428118</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230331072518.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2015 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s13351-015-5036-4</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR031428118</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s13351-015-5036-4-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhou, Tianjun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Uncertainty in the 2°C warming threshold related to climate sensitivity and climate feedback</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Climate sensitivity is an important index that measures the relationship between the increase in greenhouse gases and the magnitude of global warming. Uncertainties in climate change projection and climate modeling are mostly related to the climate sensitivity. The climate sensitivities of coupled climate models determine the magnitudes of the projected global warming. In this paper, the authors thoroughly review the literature on climate sensitivity, and discuss issues related to climate feedback processes and the methods used in estimating the equilibrium climate sensitivity and transient climate response (TCR), including the TCR to cumulative $ CO_{2} $ emissions. After presenting a summary of the sources that affect the uncertainty of climate sensitivity, the impact of climate sensitivity on climate change projection is discussed by addressing the uncertainties in 2°C warming. 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