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	<id>https://www.iamcdocumentation.eu/history/Modelling_of_climate_indicators_-_C3IAM?feed=atom</id>
	<title>Modelling of climate indicators - C3IAM - Revision history</title>
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	<updated>2026-06-25T14:47:34Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14948&amp;oldid=prev</id>
		<title>Qiao-Mei Liang at 12:11, 5 August 2021</title>
		<link rel="alternate" type="text/html" href="https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14948&amp;oldid=prev"/>
		<updated>2021-08-05T12:11:25Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 14:11, 5 August 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l4&quot;&gt;Line 4:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 4:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate module represents the climate component, and the emission information generated from C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/GEEPA is fed into C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate. We used C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate to calculate climate indicators such as global mean temperature changes and radiative forcing. Here the Climate module is developed according to the Beijing Climate Center Climate System Model (BCC_CSM), which is one of the earth system models that participated in CMIP5 simulations for the IPCC AR5 (see Figure 1 for the framework). The BCC_CSM has four component models, i.e., Global Atmosphere Model (BCC_AGCM2.1), Land Surface Model (BCC_AVIM1.0), Global Ocean Model (MOM4_L40v1) and Global Thermodynamic Sea Ice Model (SIS). These component models are inter-related and interacted with each other through fluxes of energy, momentum and water. The flux coupler was based on that of NCAR/CCSM2. The BCC_CSM is a fully coupled Climate–Carbon Cycle Model, including oceanic and terrestrial carbon cycle with dynamical vegetation. The atmospheric CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; concentration and its temporal evolution can be well reproduced when forced by anthropogenic emissions of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;. In addition to the long-term climate change simulations and projections, BCC_CSM has also been used for short-term climate predictions, as well as the Sub-seasonal to Seasonal (S2S) Prediction Project.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate module represents the climate component, and the emission information generated from C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/GEEPA is fed into C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate. We used C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate to calculate climate indicators such as global mean temperature changes and radiative forcing. Here the Climate module is developed according to the Beijing Climate Center Climate System Model (BCC_CSM), which is one of the earth system models that participated in CMIP5 simulations for the IPCC AR5 (see Figure 1 for the framework). The BCC_CSM has four component models, i.e., Global Atmosphere Model (BCC_AGCM2.1), Land Surface Model (BCC_AVIM1.0), Global Ocean Model (MOM4_L40v1) and Global Thermodynamic Sea Ice Model (SIS). These component models are inter-related and interacted with each other through fluxes of energy, momentum and water. The flux coupler was based on that of NCAR/CCSM2. The BCC_CSM is a fully coupled Climate–Carbon Cycle Model, including oceanic and terrestrial carbon cycle with dynamical vegetation. The atmospheric CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; concentration and its temporal evolution can be well reproduced when forced by anthropogenic emissions of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;. In addition to the long-term climate change simulations and projections, BCC_CSM has also been used for short-term climate predictions, as well as the Sub-seasonal to Seasonal (S2S) Prediction Project.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:8.png|Figure 1. The framework of BCC_CSM&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|frame&lt;/del&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:8.png&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|left|900px|thumb&lt;/ins&gt;|Figure 1. The framework of BCC_CSM]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Qiao-Mei Liang</name></author>
	</entry>
	<entry>
		<id>https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14889&amp;oldid=prev</id>
		<title>Mathijs Harmsen at 14:00, 3 August 2021</title>
		<link rel="alternate" type="text/html" href="https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14889&amp;oldid=prev"/>
		<updated>2021-08-03T14:00:14Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 16:00, 3 August 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l4&quot;&gt;Line 4:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 4:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate module represents the climate component, and the emission information generated from C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/GEEPA is fed into C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate. We used C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate to calculate climate indicators such as global mean temperature changes and radiative forcing. Here the Climate module is developed according to the Beijing Climate Center Climate System Model (BCC_CSM), which is one of the earth system models that participated in CMIP5 simulations for the IPCC AR5 (see Figure 1 for the framework). The BCC_CSM has four component models, i.e., Global Atmosphere Model (BCC_AGCM2.1), Land Surface Model (BCC_AVIM1.0), Global Ocean Model (MOM4_L40v1) and Global Thermodynamic Sea Ice Model (SIS). These component models are inter-related and interacted with each other through fluxes of energy, momentum and water. The flux coupler was based on that of NCAR/CCSM2. The BCC_CSM is a fully coupled Climate–Carbon Cycle Model, including oceanic and terrestrial carbon cycle with dynamical vegetation. The atmospheric CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; concentration and its temporal evolution can be well reproduced when forced by anthropogenic emissions of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;. In addition to the long-term climate change simulations and projections, BCC_CSM has also been used for short-term climate predictions, as well as the Sub-seasonal to Seasonal (S2S) Prediction Project.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate module represents the climate component, and the emission information generated from C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/GEEPA is fed into C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate. We used C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate to calculate climate indicators such as global mean temperature changes and radiative forcing. Here the Climate module is developed according to the Beijing Climate Center Climate System Model (BCC_CSM), which is one of the earth system models that participated in CMIP5 simulations for the IPCC AR5 (see Figure 1 for the framework). The BCC_CSM has four component models, i.e., Global Atmosphere Model (BCC_AGCM2.1), Land Surface Model (BCC_AVIM1.0), Global Ocean Model (MOM4_L40v1) and Global Thermodynamic Sea Ice Model (SIS). These component models are inter-related and interacted with each other through fluxes of energy, momentum and water. The flux coupler was based on that of NCAR/CCSM2. The BCC_CSM is a fully coupled Climate–Carbon Cycle Model, including oceanic and terrestrial carbon cycle with dynamical vegetation. The atmospheric CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; concentration and its temporal evolution can be well reproduced when forced by anthropogenic emissions of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;. In addition to the long-term climate change simulations and projections, BCC_CSM has also been used for short-term climate predictions, as well as the Sub-seasonal to Seasonal (S2S) Prediction Project.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:8.png&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|thumb&lt;/del&gt;|Figure 1. The framework of BCC_CSM]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:8.png|Figure 1. The framework of BCC_CSM&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|frame&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Mathijs Harmsen</name></author>
	</entry>
	<entry>
		<id>https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14865&amp;oldid=prev</id>
		<title>Qiao-Mei Liang at 03:03, 28 June 2021</title>
		<link rel="alternate" type="text/html" href="https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14865&amp;oldid=prev"/>
		<updated>2021-06-28T03:03:50Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 05:03, 28 June 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l4&quot;&gt;Line 4:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 4:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate module represents the climate component, and the emission information generated from C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/GEEPA is fed into C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate. We used C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate to calculate climate indicators such as global mean temperature changes and radiative forcing. Here the Climate module is developed according to the Beijing Climate Center Climate System Model (BCC_CSM), which is one of the earth system models that participated in CMIP5 simulations for the IPCC AR5 (see Figure 1 for the framework). The BCC_CSM has four component models, i.e., Global Atmosphere Model (BCC_AGCM2.1), Land Surface Model (BCC_AVIM1.0), Global Ocean Model (MOM4_L40v1) and Global Thermodynamic Sea Ice Model (SIS). These component models are inter-related and interacted with each other through fluxes of energy, momentum and water. The flux coupler was based on that of NCAR/CCSM2. The BCC_CSM is a fully coupled Climate–Carbon Cycle Model, including oceanic and terrestrial carbon cycle with dynamical vegetation. The atmospheric CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; concentration and its temporal evolution can be well reproduced when forced by anthropogenic emissions of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;. In addition to the long-term climate change simulations and projections, BCC_CSM has also been used for short-term climate predictions, as well as the Sub-seasonal to Seasonal (S2S) Prediction Project.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate module represents the climate component, and the emission information generated from C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/GEEPA is fed into C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate. We used C&amp;lt;sup&amp;gt;3&amp;lt;/sup&amp;gt;IAM/Climate to calculate climate indicators such as global mean temperature changes and radiative forcing. Here the Climate module is developed according to the Beijing Climate Center Climate System Model (BCC_CSM), which is one of the earth system models that participated in CMIP5 simulations for the IPCC AR5 (see Figure 1 for the framework). The BCC_CSM has four component models, i.e., Global Atmosphere Model (BCC_AGCM2.1), Land Surface Model (BCC_AVIM1.0), Global Ocean Model (MOM4_L40v1) and Global Thermodynamic Sea Ice Model (SIS). These component models are inter-related and interacted with each other through fluxes of energy, momentum and water. The flux coupler was based on that of NCAR/CCSM2. The BCC_CSM is a fully coupled Climate–Carbon Cycle Model, including oceanic and terrestrial carbon cycle with dynamical vegetation. The atmospheric CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; concentration and its temporal evolution can be well reproduced when forced by anthropogenic emissions of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;. In addition to the long-term climate change simulations and projections, BCC_CSM has also been used for short-term climate predictions, as well as the Sub-seasonal to Seasonal (S2S) Prediction Project.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[File:8.png|thumb|Figure 1. The framework of BCC_CSM]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Qiao-Mei Liang</name></author>
	</entry>
	<entry>
		<id>https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14863&amp;oldid=prev</id>
		<title>Qiao-Mei Liang at 03:02, 28 June 2021</title>
		<link rel="alternate" type="text/html" href="https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14863&amp;oldid=prev"/>
		<updated>2021-06-28T03:02:49Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 05:02, 28 June 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l3&quot;&gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;|DocumentationCategory=Modelling of climate indicators&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;|DocumentationCategory=Modelling of climate indicators&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The C&amp;lt;sup&gt;3&amp;lt;/sup&gt;IAM/Climate module represents the climate component, and the emission information generated from C&amp;lt;sup&gt;3&amp;lt;/sup&gt;IAM/GEEPA is fed into C&amp;lt;sup&gt;3&amp;lt;/sup&gt;IAM/Climate. We used C&amp;lt;sup&gt;3&amp;lt;/sup&gt;IAM/Climate to calculate climate indicators such as global mean temperature changes and radiative forcing. Here the Climate module is developed according to the Beijing Climate Center Climate System Model (BCC_CSM), which is one of the earth system models that participated in CMIP5 simulations for the IPCC AR5 (see Figure 1 for the framework). The BCC_CSM has four component models, i.e., Global Atmosphere Model (BCC_AGCM2.1), Land Surface Model (BCC_AVIM1.0), Global Ocean Model (MOM4_L40v1) and Global Thermodynamic Sea Ice Model (SIS). These component models are inter-related and interacted with each other through fluxes of energy, momentum and water. The flux coupler was based on that of NCAR/CCSM2. The BCC_CSM is a fully coupled Climate–Carbon Cycle Model, including oceanic and terrestrial carbon cycle with dynamical vegetation. The atmospheric CO&amp;lt;sub&gt;2&amp;lt;/sub&gt; concentration and its temporal evolution can be well reproduced when forced by anthropogenic emissions of CO&amp;lt;sub&gt;2&amp;lt;/sub&gt;. In addition to the long-term climate change simulations and projections, BCC_CSM has also been used for short-term climate predictions, as well as the Sub-seasonal to Seasonal (S2S) Prediction Project.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Qiao-Mei Liang</name></author>
	</entry>
	<entry>
		<id>https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14798&amp;oldid=prev</id>
		<title>Mathijs Harmsen: Edited automatically from page C3IAM setup.</title>
		<link rel="alternate" type="text/html" href="https://www.iamcdocumentation.eu/index.php?title=Modelling_of_climate_indicators_-_C3IAM&amp;diff=14798&amp;oldid=prev"/>
		<updated>2021-06-23T10:06:00Z</updated>

		<summary type="html">&lt;p&gt;Edited automatically from page &lt;a href=&quot;/C3IAM_setup&quot; title=&quot;C3IAM setup&quot;&gt;C3IAM setup&lt;/a&gt;.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{ModelDocumentationTemplate&lt;br /&gt;
|IsDocumentationOf=C3IAM&lt;br /&gt;
|DocumentationCategory=Modelling of climate indicators&lt;br /&gt;
}}&lt;/div&gt;</summary>
		<author><name>Mathijs Harmsen</name></author>
	</entry>
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