pmip3:design:lm:final
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pmip3:design:lm:final [2010/08/02 16:35] – Change, and added links for all doi references jypeter | pmip3:design:lm:final [2014/10/02 22:05] (current) – [Vegetation] kaplan | ||
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- | //Go to =>// [ [[pmip3: | + | //Go to =>// [ [[pmip3: |
====== Last Millennium Experimental Design ====== | ====== Last Millennium Experimental Design ====== | ||
- | The basic principle is that we should strive to include all relevant transient forcings over this period if the functionality exists in the model, noting that conformability with the CMIP5 controls and 20th Century transient is crucial. | + | The basic principle is that we should strive to include all relevant transient forcings over this period if the functionality exists in the model, noting that conformability with the CMIP5 controls and 20th Century transient is crucial. |
+ | |||
+ | <note important> | ||
+ | [[http:// | ||
+ | |||
+ | //G. A. Schmidt, J. H. Jungclaus, C. M. Ammann, E. Bard, P. Braconnot, T. J. Crowley, G. Delaygue, F. Joos, N. A. Krivova, R. Muscheler, B. L. Otto-Bliesner, | ||
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+ | </ | ||
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+ | ===== Participants ===== | ||
+ | |||
+ | <note important> | ||
===== Boundary conditions ===== | ===== Boundary conditions ===== | ||
+ | |||
==== Summary of Last Millennium boundary conditions ==== | ==== Summary of Last Millennium boundary conditions ==== | ||
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The stratospheric aerosol loadings (in units of Tg) provided in the IVI2 data set may be converted into aerosol optical depth (AOD) by dividing the loadings by 150 Tg (Stothers, 1984). The AOD time series can then be used to calculate the corresponding radiative forcing (in units of Wm-2) by multiplying it by (-20) (Wigley et al., 2005). The conversion to AOD is valid for aerosols with effective radius in the visible spectral range. | The stratospheric aerosol loadings (in units of Tg) provided in the IVI2 data set may be converted into aerosol optical depth (AOD) by dividing the loadings by 150 Tg (Stothers, 1984). The AOD time series can then be used to calculate the corresponding radiative forcing (in units of Wm-2) by multiplying it by (-20) (Wigley et al., 2005). The conversion to AOD is valid for aerosols with effective radius in the visible spectral range. | ||
- | Further explanation is provided here : {{: | + | Note: the '' |
Gao, C., A. Robock, and C. Ammann: Volcanic forcing of climate over the last 1500 years: An improved ice-core based index for climate models. J. Geophys. Res., 113, D2311, doi: | Gao, C., A. Robock, and C. Ammann: Volcanic forcing of climate over the last 1500 years: An improved ice-core based index for climate models. J. Geophys. Res., 113, D2311, doi: | ||
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| PERI-180 | | PERI-180 | ||
- | ==== Vegetation ==== | + | ==== Land Cover: Natural |
- | Anthropogenic land cover change is considered by applying | + | Anthropogenic land cover change is considered by applying |
- | The global | + | === Pongratz 2008 === |
+ | |||
+ | Global | ||
The data set can be obtained from the World Data Center for Climate (doi: | The data set can be obtained from the World Data Center for Climate (doi: | ||
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To access the files, click here [[http:// | To access the files, click here [[http:// | ||
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+ | === KK10 === | ||
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+ | The following alternative anthropogenic land use forcing data set has been provided by [[jed.kaplan@unil.ch|Jed Kaplan]] | ||
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+ | [[http:// | ||
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+ | Kaplan, J. O., Krumhardt, K. M., Ellis, E. C., Ruddiman, W. F., Lemmen, C. and Goldewijk, K. K. 2010. Holocene carbon emissions as a result of anthropogenic land cover change. The Holocene, 21(5), 775-791, doi: | ||
===== Initial conditions ===== | ===== Initial conditions ===== | ||
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===== Links ===== | ===== Links ===== | ||
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+ | * [[http:// | ||
* PCMIP Project (**P**alaeo**C**arbon **M**odelling **I**ntercomparison **P**roject)\\ http:// | * PCMIP Project (**P**alaeo**C**arbon **M**odelling **I**ntercomparison **P**roject)\\ http:// |
pmip3/design/lm/final.1280759711.txt.gz · Last modified: 2010/08/02 16:35 by jypeter