Kees Klein Goldewijk provided updates on
his early global land use reconstructions (HYDE going to 3.2 & 4.0).
Not exact matches
All of this work will soon be advanced enormously by a major new collaborative international working group led by Kathleen Morrison,
Land Use 6000 (LU6K), which aims to provide empirical global reconstructions of land use and land cover over the past 6000 years and earlier as part of the Land Cover 6000 project (LC6K) of PA
Land Use 6000 (LU6K), which aims to provide empirical global reconstructions of land use and land cover over the past 6000 years and earlier as part of the Land Cover 6000 project (LC6K) of PAG
Use 6000 (LU6K), which aims to provide empirical
global reconstructions of
land use and land cover over the past 6000 years and earlier as part of the Land Cover 6000 project (LC6K) of PA
land use and land cover over the past 6000 years and earlier as part of the Land Cover 6000 project (LC6K) of PAG
use and
land cover over the past 6000 years and earlier as part of the Land Cover 6000 project (LC6K) of PA
land cover over the past 6000 years and
earlier as part of the
Land Cover 6000 project (LC6K) of PA
Land Cover 6000 project (LC6K) of PAGES.
New
global land use datasets are being developed that indicate that human
use of
land may have been far more extensive at much
earlier times - most of the terrestrial biosphere may have been transformed by humans long before the 20th century - maybe even by 3000 years ago!
An
early 2008 study led by Tim Searchinger of Princeton University that was published in Science
used a
global agricultural model to show that when including the
land clearing in the tropics, expanding U.S. biofuel production increased annual greenhouse gas emissions dramatically instead of reducing them, as more narrowly based studies claimed.
If our assumed
land use changes occur a decade
earlier, CO2 returns to 350 ppm several years
earlier; however that has negligible effect on the maximum
global temperature calculated below.
Although these new
global land -
use histories remain at an
early stage of development, their quantitative and spatially detailed
global predictions offer an unprecedented opportunity to investigate the
global extent, timing, driving forces, and impacts of
land use as a process transforming the Earth System over the Holocene.
As a result of this emphasis and the prior absence of adequate tools, theory, and data, quantitative
global land -
use histories for
earlier periods of the Holocene have only recently been developed (4, 19 ⇓ — 21).
The
Early Anthropogenic Hypothesis (108) posits that mid-Holocene increases in CO2 and CH4 resulted from early land clearing and other agricultural practices and that these unprecedented interglacial trends in atmospheric composition set global climate on a trajectory toward warmer conditions long before human use of fossil fuels (108,
Early Anthropogenic Hypothesis (108) posits that mid-Holocene increases in CO2 and CH4 resulted from
early land clearing and other agricultural practices and that these unprecedented interglacial trends in atmospheric composition set global climate on a trajectory toward warmer conditions long before human use of fossil fuels (108,
early land clearing and other agricultural practices and that these unprecedented interglacial trends in atmospheric composition set
global climate on a trajectory toward warmer conditions long before human
use of fossil fuels (108, 109).
Regardless of whether
early land use significantly affected
global climate, understanding the
global role of
land use in determining the onset and magnitude of anthropogenic climate change is critical for gauging the climatic impact of current and future modifications of the terrestrial biosphere, including efforts to offset fossil fuel emissions by reducing deforestation (114).
This analytical document captures
early observations in engaging the private sector, particularly multinational companies involved in
global agricultural commodity supply chains, in the context of emission reductions programs to address
land use change.