Global Change Master Directorygsfc-gcmduso@mail.nasa.gov502013-06-20T05:13:11ZGCMD Search: Parameters|PALEOCLIMATE|PALEOCLIMATE RECONSTRUCTIONS|VEGETATION RECONSTRUCTIONhttp://mddemo.gsfc.nasa.gov/KeywordSearch/OpenSearch.do 45 0 http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_94-007Mapping Eastern North America Vegetation Change Over the Past 18,000 Years-90.0,20.0,-50.0,65.02012-08-31T04:00:00ZThese maps are based on 11,700 fossil pollen samples and 1744 modern pollen
samples. Twenty-one pollen taxa were included in analyses: Alnus, Fraxinum,
Populus, Tilia, Fagus, Betula, Ulmus, Abies, ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]USGS_CLUESClimate, Land Use, and Environmental Sensitivity (CLUES)-168.0,9.0,-52.0,80.02011-09-29T04:00:00ZVegetation changes caused by climatic variations and/or land use may have large impacts on forests, agriculture, rangelands, natural ecosystems, and endangered species. Climate modeling studies indicate ...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]miller_0126146Late Paleozoic-Mesozoic fauna, environment, climate, Beardmore Glacier area171.0,-83.75,171.0,-83.752003-11-18T00:00:00Z2003-12-21T00:00:00Z2010-07-09T04:00:00ZThe 4 km thick sequence of sedimentary rocks in the Beardmore Glacier area records 90 million years of Permian through Jurassic history of this high-paleolatitude sector of Gondwana. It accumulated ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]ANT-0739700_BU-054-004Collaborative Research: Integrating Geomorphological and Paleoecological Studies to Reconstruct Neogene Environments of the Transantarctic Mountains 160.0,-78.5,164.5,-76.52010-07-02T04:00:00ZThis project studies the last vestiges of life in Antarctica from exceptionally well-preserved fossils of tundra life--mosses, diatoms, ostracods, Nothofagus leaves, wood, and insect remains recently ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]Warny-OPPGeol-0533879Feasibility Study of Eocene to Pliocene Palynological Reconstruction off Seymour Island-54.0,-65.0,-58.0,-62.02005-03-01T00:00:00Z2007-02-28T00:00:00Z2010-07-02T04:00:00ZFeasibility study of Eocene to Pliocene palynological reconstruction of the
Antarctic Peninsula margin climate evolution
Project Summary
Intellectual merit
Numerous ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]ANT-0440711_BU-054-003Fossil-rich lacustrine deposits in the Dry Valleys, Antarctica 160.0,-78.5,164.5,-76.52010-07-02T04:00:00ZThe data set includes fossil images,trace-element geochemical analyses of volcanic tephra, geochronologic data for Dry Valleys ashfall deposits, locations and description of soil pits in the Antarctic ...http://gcmd.gsfc.nasa.gov/getdif.htm?[BAS_AEDC]GB-NERC-BAS-AEDC-00311AFI 01/01_01 - Biodiversity response to climate change: biodiversity and climate significance of Tertiary forest communities of Antarctica - Fossil wood and leaves of Tertiary age, Seymour Island and adjacent, 2001-56.75,-64.283,-56.75,-64.2832001-01-01T00:00:00Z2001-03-31T00:00:00Z2010-04-27T04:00:00ZDuring field work in 2001 over 1600 specimens were collected from four main fossil plant assemblages: the ''Nordenksjold flora'' from the Cross Valley Formation of Late Palaeocene age; and 3 floras ...http://gcmd.gsfc.nasa.gov/getdif.htm?[BAS_AEDC]GB-NERC-BAS-AEDC-00312AFI 01/01_02 - Biodiversity response to climate change: biodiversity and climate significance of Tertiary forest communities of Antarctica - Analysis of fossil wood & leaves of Tertiary age, Seymour Island&adjacent, 2001-56.75,-64.283,-56.75,-64.2832000-08-14T00:00:00Z2003-02-13T00:00:00Z2010-04-27T04:00:00ZFossils from Palaeogene strata on Seymour Island, Antarctic Peninsula, were studied to determine the nature of vegetation response to the fundamental change from greenhouse to icehouse climates in ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]K042_1997_1998_NZ_1Investigation of petrified logs, palaeobotanical materical and tree growth rings from Allan Hills for intrepretation of the palaeoclimate of the area159.4167,-76.8333,160.0,-76.58331997-12-09T00:00:00Z1997-12-19T00:00:00Z2009-06-02T04:00:00ZAllan Hills is known for its record of climate preserved in petrified logs 260 million years old in the Wellar coal measure. A study of the logs is part of a wider study on ancient forests in Jurassic ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]MBG_vastThe Missouri Botanical Garden Nomenclatural Database -180.0,-23.0,178.0,36.02009-05-08T04:00:00ZThe Missouri Botanical Garden (MOBOT) makes available a variety of data for
vascular plants throughout the globe. W3TROPICOS is a catalogue of specimens
and species information. It ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2001-046BIOME 6000: Reconstructed Biomes from Palaeoecological Data-180.0,-90.0,180.0,90.02009-04-20T04:00:00ZThe Global Palaeovegetation Mapping (BIOME 6000) Project is a community-wide
collaboration inaugurated in 1994 under the joint auspices of four of the
elements of the International Geosphere-Biosphere ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]USGS_OF99-535Middle Pliocene Paleoenvironmental Reconstruction: PRISM2-180.0,-90.0,180.0,90.02009-03-24T04:00:00ZAs part of the USGS Global Change Research effort, the PRISM (Pliocene Research, Interpretation and Synoptic Mapping) Project has documented the characteristics of middle Pliocene climate on a ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]INTERGLACIAL_LAND_MAPSGlobal Land Environments since the Last Interglacial, Compiled by Jonathan Adams-180.0,-90.0,180.0,90.02008-05-30T04:00:00ZThe paleo-ecosystems maps are based on simple compilations of the available information in the literature, relying heavily on the conclusions given by review papers for each subregion. Dates are given ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_IMPDThe International Multiproxy Paleofire Database (IMPD) at WDC for Paleoclimatology-180.0,-90.0,-180.0,90.00600-01-01T00:00:00ZT00:00:00Z2007-09-11T04:00:00ZFrom: A Brief Introduction to Fire History Reconstruction
"http://www.ncdc.noaa.gov/paleo/impd/impd_data_intro.html"
Fire history information is provided through two types of proxy data; tree-ring ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]PALEOMAPThe PALEOMAP Project: Paleogeographic Atlas, Plate Tectonic Software, and Paleoclimate Reconstructions-180.0,-90.0,180.0,90.02007-01-31T05:00:00ZThe PALEOMAP project produces paleogreographic maps illustrating the
Earth's plate tectonic, paleogeographic, climatic, oceanographic and
biogeographic development from the Precambrian to the Modern ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]FE01020CLIMAP 18k bp Surface Configuration Data-180.0,-90.0,180.0,90.02006-12-18T05:00:00ZThe CLIMAP (Climate: Long-Range Investigation, Mapping, and
Prediction) Project was funded by the National Science Foundation as
part of the International Decade of Ocean Exploration (IDOE). The ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2000-024Southern Ocean Biomarker Flux Data Set 146.87,-48.14,146.87,-48.142006-12-14T05:00:00ZThis data set consists of marine and terrestrial biomarker data used for
paleoenvironmental reconstruction of atmospheric transport and
glacial-interglacial marine productivity changes.http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]CDIAC_NDP11Global Paleoclimatic Data for 6000 Year B.P., CDIAC NDP-011-180.0,-90.0,180.0,90.02006-12-13T05:00:00ZThe data set consists of pollen, lake level, marine plankton data and, where
possible, quantitative values estimated from these data gathered from 797
stations. The reasons for choosing these three ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_2003-089Late Quaternary North American Vegetation Dynamics Data-180.0,5.0,-20.0,90.02006-12-13T05:00:00ZThis paper integrates the mapping of late-Quaternary biomes with palynological
evidence for individualistic species responses to environmental change. We
document vegetation history in boreal and ...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]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]EARTH_LAND_NGDC_PALEO_TREERINGSTree Ring Data from the International Tree-Ring Data Bank (ITRDB), NOAA/NCDC Paleoclimatology Program-180.0,-60.0,180.0,75.02006-05-09T04:00:00ZThe International Tree-Ring Data Bank is maintained by the NOAA
Paleoclimatology Program and World Data Center for
Paleoclimatology. The Data Bank includes raw ring width or wood
density measurements, ...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 ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NCDC_PALEO_96-022European Land Surface Conditions 6K Reconstruction-10.0,35.0,60.0,75.02005-04-20T04:00:00ZThese biomes are interpolated from 2014 pollen surface samples, for the
Present, and from 343 pollen sites for 6000 yr BP. The coverage is relatively
well balanced for the modern data, but the region ...http://gcmd.gsfc.nasa.gov/getdif.htm?[GCMD]NOAA_NGDC_PALEO_AFRICA6KAfrican 6000 Years B.P. Land Surface Conditions, WDC Paleoclimatology-17.0,10.0,60.0,30.02005-04-19T04:00:00ZThis dataset describes land surface conditions at 6000 years B.P. on a
1 degree x 1 degree grid across northern Africa and the Arabian
Peninsula. It includes information on the percentage in each ...