2006
DOI: 10.1029/2006jd007366
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ISLSCP Initiative II global data sets: Surface boundary conditions and atmospheric forcings for land‐atmosphere studies

Abstract: We report herein the publication and evaluation of the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II global interdisciplinary data record. The record consists of 52 data sets, with a common series in the 10‐year period 1985 to 1996. Selected data series extend well beyond this period. All series are coregistered to a common grid and gap‐filled for continuity using uniform procedures. We describe briefly the individual data sets within the collection; provide user guidance; and… Show more

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Cited by 68 publications
(61 citation statements)
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“…Northern hemispheric monthly snow cover extent data (Armstrong and Brodzik, 2010) from the International Satellite Land-Surface Climatology Project, Initiative II (ISLSCP II) (Hall et al, 2006) together with the monthly masks of maximum sea ice extent derived by the National Snow and Ice Data Center (NSIDC) from the sea ice concentrations obtained from passive microwave data (Cavalieri et al, 1996) were used to determine the days of year when snow or ice was present in each grid cell. The monthly Minimum Lambert Equivalent Reflectivity (MLER) climatology (Herman and Celarier, 1997) is then used for regions and time periods with permanent or negligible snow/ice cover while a climatology better capturing the seasonal changes in the surface albedo during the snow/ice melting and formation periods (Tanskanen et al, 2004) is used elsewhere.…”
Section: Surface Albedo and Aerosol Climatologiesmentioning
confidence: 99%
“…Northern hemispheric monthly snow cover extent data (Armstrong and Brodzik, 2010) from the International Satellite Land-Surface Climatology Project, Initiative II (ISLSCP II) (Hall et al, 2006) together with the monthly masks of maximum sea ice extent derived by the National Snow and Ice Data Center (NSIDC) from the sea ice concentrations obtained from passive microwave data (Cavalieri et al, 1996) were used to determine the days of year when snow or ice was present in each grid cell. The monthly Minimum Lambert Equivalent Reflectivity (MLER) climatology (Herman and Celarier, 1997) is then used for regions and time periods with permanent or negligible snow/ice cover while a climatology better capturing the seasonal changes in the surface albedo during the snow/ice melting and formation periods (Tanskanen et al, 2004) is used elsewhere.…”
Section: Surface Albedo and Aerosol Climatologiesmentioning
confidence: 99%
“…This value yields soil bucket depths that are a reasonably good fit with a plant-available water dataset based on optimal rooting depths (Kleidon and Heimann, 1998;Hall et al, 2006;Kleidon, 2011). In that dataset, the soil bucket depths in the most sparsely vegetated regions range from around 0.05 m in the Canadian polar desert to < 0.003 m in the hyperarid Atacama and northeast Sahara deserts.…”
Section: Soil Bucket Depthmentioning
confidence: 84%
“…2.3.2) gives generally much lower values (not shown) in the wet and dry tropics than in the reference dataset (Kleidon and Heimann, 1998;Hall et al, 2006;Kleidon, 2011). Such lower values of soil waterholding capacity should lead one to expect a positive runoff bias in these areas in SEDGES.…”
Section: Evaluation Of Evapotranspiration and Runoffmentioning
confidence: 99%
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“…Global 1°gridded data set of 18 selected soil parameters including maximum soil available water content (M awc ) for a soil depth of 0-150 cm, downloaded from the Oak Ridge National Laboratory Distributed Active Archive Center (ORNL DAAC) (http://daac.ornl.gov/) by this study, was developed by the International Satellite Land Surface Climatology Project (ISLSCP) Initiative II project based on the International GeosphereBiosphere Programme-Data and Information Services soil data [Hall et al, 2006].…”
Section: Islscp II Global Gridded Soil Datamentioning
confidence: 99%