Results 41 to 50 of about 17,582,102 (249)

Variable particle size distributions reduce the sensitivity of global export flux to climate change [PDF]

open access: yesBiogeosciences, 2021
Recent earth system models predict a 10 %–20 % decrease in particulate organic carbon export from the surface ocean by the end of the 21st century due to global climate change. This decline is mainly caused by increased stratification of the upper ocean,
S. W. Leung   +5 more
doaj   +1 more source

Quantifying the impact of ocean acidification on our future climate [PDF]

open access: yesBiogeosciences, 2014
Ocean acidification (OA) is the consequence of rising atmospheric CO2 levels, and it is occurring in conjunction with global warming. Observational studies show that OA will impact ocean biogeochemical cycles. Here, we use an Earth system model under the
R. J. Matear, A. Lenton
doaj   +1 more source

Fluvial sedimentary deposits as carbon sinks: organic carbon pools and stabilization mechanisms across a Mediterranean catchment [PDF]

open access: yesBiogeosciences, 2019
The role of fluvial sedimentary areas as organic carbon sinks remains largely unquantified. Little is known about mechanisms of organic carbon (OC) stabilization in alluvial sediments in semiarid and subhumid catchments where those mechanisms are quite ...
M. Martínez-Mena   +5 more
doaj   +1 more source

Historical CO2 emissions from land use and land cover change and their uncertainty [PDF]

open access: yesBiogeosciences, 2020
Emissions from land use and land cover change are a key component of the global carbon cycle. However, models are required to disentangle these emissions from the land carbon sink, as only the sum of both can be physically observed.
T. Gasser   +7 more
doaj   +1 more source

Ideas and perspectives: is shale gas a major driver of recent increase in global atmospheric methane? [PDF]

open access: yesBiogeosciences, 2019
Methane has been rising rapidly in the atmosphere over the past decade, contributing to global climate change. Unlike the late 20th century when the rise in atmospheric methane was accompanied by an enrichment in the heavier carbon stable isotope (13C ...
R. W. Howarth
doaj   +1 more source

Evaluation of Oxfam GB's Climate Change Campaign [PDF]

open access: yes, 2010
This evaluation looks at Oxfam GB's global climate change campaign with in-depth case studies from Bangladesh, South Africa and the UK. The evaluation covers the period from March 2008 to December 2009, although the majority of available documentation ...
Otero, Eva
core   +1 more source

Climate engineering and the ocean: effects on biogeochemistry and primary production [PDF]

open access: yesBiogeosciences, 2017
Here we use an Earth system model with interactive biogeochemistry to project future ocean biogeochemistry impacts from the large-scale deployment of three different radiation management (RM) climate engineering (also known as geoengineering) methods:
S. K. Lauvset, J. Tjiputra, H. Muri
doaj   +1 more source

Patterns and persistence of hydrologic carbon and nutrient export from collapsing upland permafrost [PDF]

open access: yesBiogeosciences, 2015
As high latitudes warm, vast stocks of carbon and nitrogen stored in permafrost will become available for transport to aquatic ecosystems. While there is a growing understanding of the potential effects of permafrost collapse (thermokarst) on aquatic ...
B. W. Abbott   +4 more
doaj   +1 more source

Benchmarking and parameter sensitivity of physiological and vegetation dynamics using the Functionally Assembled Terrestrial Ecosystem Simulator (FATES) at Barro Colorado Island, Panama [PDF]

open access: yesBiogeosciences, 2020
Plant functional traits determine vegetation responses to environmental variation, but variation in trait values is large, even within a single site. Likewise, uncertainty in how these traits map to Earth system feedbacks is large.
C. D. Koven   +33 more
doaj   +1 more source

Increase of dissolved inorganic carbon and decrease in pH in near-surface waters in the Mediterranean Sea during the past two decades [PDF]

open access: yesBiogeosciences, 2018
Two 3-year time series of hourly measurements of the fugacity of CO2 (fCO2) in the upper 10 m of the surface layer of the northwestern Mediterranean Sea have been recorded by CARIOCA sensors almost two decades apart, in 1995–1997 and 2013–2015.
L. Merlivat   +6 more
doaj   +1 more source

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