Global Change Master Directorygsfc-gcmduso@mail.nasa.gov502013-05-25T02:46:54ZGCMD Search: Projects|P - R|PMIPhttp://mddemo.gsfc.nasa.gov/KeywordSearch/OpenSearch.do 28 0 http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]LGM_TROPICALTropical Climates At The Last Glacial Maximum-180.0,-90.0,180.0,90.02011-04-08T04:00:00ZThe LGM Tropical Terrestrial Data Synthesis (Farrera et al., 1999) contains
quantitative reconstructions of mean temperature of the coldest month (MTCO)
and mean annual ground temperature ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]6K_N_ATLANTIC_SST6k North Atlantic Sea-Surface Temperatures-180.0,-90.0,180.0,90.02011-04-07T04:00:00ZThe 6k data are based on two types of data: 1) alkenones, a geochemical proxy,
and 2) transfer function estimates of sea-surface temperature based on faunal
assemblages of planktic foraminifers. All ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]GLSDBGlobal Lake Status Data Base (GLSDB)-180.0,-90.0,180.0,90.02009-05-08T04:00:00ZThe Global Lake Status Data Base (GLSDB: Kohfeld and Harrison, 2000, Harrison
et al., 2003) is a long-standing international effort to compile the geomorphic
and biostratigraphic data ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP2_TROPICALCLIMDiagnostic For Magnitude Of Tropical Cooling At Last Glacial Maximum-180.0,-90.0,180.0,90.02009-01-21T05:00:00ZThe LGM Tropical Terrestrial Data Synthesis was used as a diagnostic by Pinot
et al. (1999) and in the IPCC (2001). An updated version of this diagram was
presented by Harrison (2000). ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]EARTH_LAND_NGDC_PALEO_LAKELEVELAncient Lake Level (Caspian Sea and Aral Sea) Paleoclimate Data45.0,33.0,65.0,50.02006-09-29T04:00:00ZThe lake level dataset contains data on the reconstructed extent of the Aral
and Caspian Seas during the last glacial maximum 18,000 YBP. The
reconstructions were made by Olga Dennisenko (Department ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]BIOME6000BIOME 6000 (v4.2): Vegetation Maps for the Mid-Holocene and Last Glacial Maximum-180.0,-90.0,180.0,90.02006-09-26T04:00:00ZThe Palaeovegetation Mapping Project (generally known as BIOME 6000: Prentice
and Webb, 1998) was inaugurated in 1994 with the aim of providing global maps
describing the vegetation patterns at 6000?500 ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]MIDHOLO_PRECIP_NAFRICADiagnostic For Mid-Holocene Precipitation Over Northern Africa-20.0,15.0,45.0,35.02006-09-26T04:00:00ZPollen evidence indicates that grassland and xerophytic woodland/scrubland
occurred in ares of northern Africa characterised by desert today during the
mid-Holocene (Jolly et al., 1998a, 1998b). Mid-Holocene ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]BIOME6000_MEGABIOMEMega-Biome Maps for the Mid-Holocene and Last Glacial Maximum-180.0,-90.0,180.0,90.02006-09-26T04:00:00ZMost dynamic vegetation models (DGVMs) simulate far fewer PFTs, and hence
discriminate far fewer biomes, than the palaeodata allow. In order to
facilitate direct comparison with model output, we have ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIPPaleoclimate Modelling Intercomparison Project (PMIP) Model Runs-180.0,-90.0,180.0,90.02006-05-11T04:00:00ZThe Paleoclimate Modeling Intercomparison Project (PMIP) was initiated in order
to coordinate and encourage the systematic study of atmospheric general
circulation models (AGCMs) and to assess their ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_GFDLGFDL Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-07-28T04:00:00ZOne of several versions of global spectral models in use at the
Geophysical Fluid Dynamics Laboratory, ithis version of the GFDL model
is applied primarily to climate studies. In its treatment of ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_BMRCBMRC/BMRC2 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe BMRC model is a descendant of a spectral general circulation model
first developed in the 1970s (cf. Bourke et al. 1977 , and McAvaney et
al. 1978 ). This version is more recent than that used ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_CCC2CCC2 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe CCC model is the second-generation version of a model first
developed in the early 1980s for climate applications.
The model is identical to the latest AMIP model exept for different
initial ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_CCSR1CCSR1 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZModel CCSR/NIES AGCM (T21 L20) 1995 is based on a simple global
atmospheric model first developed at the University of Tokyo
(cf. Numaguti 1993), and further refined as a collaboration between
CCSR ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_CLIMBER2CLIMBER2 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZCLIMBER-2, is a model developed by the CLIMate and BiosphERe
groupe-Climate System Department at the Potsdam Institute for Climate
Impact Research (PIK).
For the PMIP, CLIMBER-2 consists of runs ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_CNRM2CNMR-2 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe model is a version (Cycle 14) of the ARPEGE climate model, which
is designed for use by the French climate community. (ARPEGE is the
acronym for Action de Recherche Petite Echelle Grande Echelle: ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_CSIROCSIRO Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe CSIRO model is derived from earlier two-level and four-level
spectral models based on the primitive equations expressed in
conservative flux form (cf. Gordon 1981, 1993 ).
For the PMIP, CSIRO ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_ECHAM3ECHAM3 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThis is the third in a series of models developed at MPI that derive
from an earlier version (cycle 17) of the operational forecast model
of the European Centre for Medium-Range Weather Forecasts ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_GEN1GEN1 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe global climate model used for PMIP is Version 1.02A of GENESIS
(Global ENvironmental and Ecological Simulation of Interactive
Systems). It has been developed at NCAR Interdisciplinary Climate ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_GEN2GEN2 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe global climate model used for PMIP is Version 2.0 of GENESIS
(Global ENvironmental and Ecological Simulation of Interactive
Systems). It has been developed at NCAR Interdisciplinary Climate
Systems ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_LMCELMD4LMCELMD4 and LMCELMD5 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZLMCELMD4:
The LMD model derives from an earlier version developed for climate
studies (cf. Sadourny and Laval 1984) . Subsequent modifications
principally include changes in the representation of ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_MRI2MRI2 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe MRI model is derived from an earlier version of the University of
California at Los Angeles (UCLA) model (cf. Arakawa and Mintz 1974 and
Arakawa and Lamb 1977 ). Subsequent modifications include ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_MSUMSU Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe MSU model was developed in 1989 for climate applications. The
latest version of this model is significantly differ from the first
version:
a) it is used the simulation with seasonal resolution, ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_GISSNASA/GISS Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe GISS model used for the PMIP experiment is a modified version of
Model II that is described by Hansen et al. (1983) . The current model
(described by Hansen et al., 1997) differs from this predecessor ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_UGAMPUGAMP Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe UGAMP model is based on the ECMWF (cycle 27) model (cf. Tiedtke et
al. 1988 and Simmons et al. 1989 ), but with modifications principally
in the treatment of radiation, convection, surface fluxes, ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_UIUC11UIUC11 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe 11-layer tropospheric/lower-stratospheric GCM is a descendent of
the 2-layer atmospheric GCM developed in the late 1960's and early
1970's by Arakawa and Mintz at UCLA , and subsequently developed ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_UKMOUKMO Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe UKMO HADAM2 model part of the line of Unified Models (UM) intended
to provide a common framework for forecasting and climate applications
(cf. Cullen 1993 ). The dynamical formulations are those ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_YONUYONU Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-20T04:00:00ZThe model extends the vertical domain and resolution of the AMIP
baseline model YONU Tr5.1 (4x5 L5) 1994 by the inclusion of 2 more
vertical levels. The method of obtaining surface values of air
temperature ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PMIP_CCM13CCM1 and CCM3 Model Runs for Paleoclimate Modelling Intercomparison Project (PMIP)-180.0,-90.0,180.0,90.02005-06-14T04:00:00ZCCM3:
The Atmospheric model is the fourth generation NCAR Community Climate Model
(version 3: CCM3). The CCM3 is an evolution of the CCM2 as described by Hack
and al (1993,1994) and CCM2 is the historical ...