Global maps of above and belowground biomass carbon density: (a) aboveground biomass carbon density, (b) belowground biomass carbon density.
Temporally consistent and harmonized global maps of aboveground and belowground biomass carbon density are now available.
Biomass (Mg ha-1) for the northern Minnesota site.
Six Landsat focus sites were used to produce disturbance history and forest biomass maps.
Forest aboveground biomass in megagrams per hectare for the year 2016.
Annual maps of aboveground biomass are available for forests in Washington, Oregon, Idaho, and western Montana, USA.
Estuaries classes used in the study: former river valley primary estuary, former glacier valley primary estuary, river delta primary estuary, tectonic structural primary estuary, coastal lagoon secondary estuary, and unclassified estuary.
Soil organic carbon (SOC) estimates and environmental data for US estuaries are available for the period 1972-2015.
Assimilated predictions of forest aboveground biomass across the Paragominas Municipality, Brazil.
Estimates of forest aboveground biomass for the Paragominas municipality, in Para, Brazil, were derived from LiDAR and PALSAR data.
Aboveground biomass mapped at 0.25 ha resolution for the Mondah study site in Gabon, West Africa.
The AfriSAR campaign produced maps of aboveground biomass for four forested sites in Gabon based on field data and LiDAR scans.
Heights of mangrove forests along the northern coast of Borneo (countries Brunei and Malaysia) reach 39 meters tall. Mangrove cover is illustrated in orange, where darker orange represents taller canopies.
Maps of the global distribution and biomass of mangrove forests are available for 116 countries.
Carbon sequestration potential within the state of Maryland, defined as 95% of maximum forest aboveground biomass (Mg/ha), simulated after 500 years of succession.
A new dataset maps the aboveground biomass of Maryland's forests and estimates their potential for future carbon sequestration.
Eurasia boreal forests aboveground carbon estimates (Neigh et al., 2013).
