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Carbon-nitrogen interactions regulate climate-carbon cycle feedbacks: results from an atmosphere-ocean general circulation model.pdf
Inclusion of fundamental ecological interactions between carbon and nitrogen cycles in the land component of an atmosphere-ocean general circulation model ...
A century of climate and ecosystem change in Western Montana: what do temperature trends portend?
Abstract The physical science linking human-induced increases ingreenhouse gasses to the warming of the global climate system is well established, but the ...
Climate commitment in an uncertain world
Climate commitment—the warming that would still occur given no further human influence—is a fundamental metric for both science and policy. It informs us of ...
Detection and Attribution of Streamflow Timing Changes to Climate Change in the Western United States
This article applies formal detection and attribution techniques to investigate the nature of observed shifts in the timing of streamflow in the western United ...
Climate Change Challenges and Opportunities for Global Health
Editorial: Journal of the American Medical Association. Health is inextricably linked to climate change. It is important for clinicians to understand this ...
Effects of Management on Carbon Sequestration in Forest Biomass in Southeast Alaska
The Tongass National Forest (Tongass) is the largest national forest and largest area of old-growth forest in the United States. Spatial geographic informa- ...
Divergent global precipitation changes induced by natural versus anthropogenic forcing
As a result of global warming, precipitation is likely to increase in high latitudes and the tropics and to decrease in already dry sub-tropical regions (1). ...
Effects of grazing on grassland soil carbon: a global review
Soils of grasslands represent a large potential reservoir for storing CO2, but this potential likely depends on how grasslands are managed for large mammal ...
Earth system sensitivity inferred from Pliocene modelling and data
Here we use a coupled atmosphere–ocean general circulation model to simulate the climate of the mid-Pliocene warm period (about three million years ago), and ...
CO2 emissions from forest loss
Deforestation is the second largest anthropogenic source of carbon dioxide to the atmosphere, after fossil fuel combustion. Following a budget reanalysis, the ...
Carbon respiration from subsurface peat accelerated by climate warming in the subarctic
Among the largest uncertainties in current projections of future climate is the feedback between the terrestrial carbon cycle and climate1. Northern peatlands ...
ESSAY : The worst-case scenario
Stephen Schneider explores what a world with 1,000 parts per million of CO2 in its atmosphere might look like.
Activation of old carbon by erosion of coastal and subsea permafrost in Arctic Siberia
The future trajectory of greenhouse gas concentrations depends on interactions between climate and the biogeosphere1,2. Thawing of Arctic permafrost could ...
Asymmetric effects of economic growth and decline on CO2 emissions
Letter to Editor: Excerpt: "Why does economic decline not have an effect on CO2 emissions that is symmetrical with the effect of economic growth? There are ...
Brownness of organics in aerosols from biomass burning linked to their black carbon content
Atmospheric particulate matter plays an important role in the Earth’s radiative balance. Over the past two decades, it has been established that a portion of ...
Ecological and Evolutionary Responses to Recent Climate Change
Ecological changes in the phenology and distribution of plants and animals are occurring in all well-studied marine, freshwater, and terrestrial groups. These ...
Combined climate and carbon-cycle effects of large-scale deforestation
The prevention of deforestation and promotion of afforestation have often been cited as strategies to slow global warming. Deforestation releases CO2 to the ...
Delayed detection of climate mitigation benefits due to climate inertia and variability
Climate change mitigation acts by reducing greenhouse gas emissions, and thus curbing, or even reversing, the increase in their atmospheric concentration. This ...
A holistic approach to climate targets
An assessment of allowable carbon emissions that factors in multiple climate targets finds smaller permissible emission budgets than those inferred from ...
Enhanced Seasonal Exchange of CO2 by Northern Ecosystems Since 1960
Seasonal variations of atmospheric carbon dioxide (CO2) in the Northern Hemisphere have increased since the 1950s, but sparse observations have prevented a ...
Amazon Basin climate under global warming: the role of the sea surface temperature
The Hadley Centre coupled climate–carbon cycle model (HadCM3LC) predicts loss of the Amazon rainforest in response to future anthropogenic greenhouse gas ...
A new, global, multi-annual (2000–2007) burnt area product at 1 km resolution Vol. 35
This paper reports on the development and validation of a new, global, burnt area product. Burnt areas are reported at a resolution of 1 km for seven fire ...
Conservation threats: biofuel
Biofuels: Europe’s largest conservation charity has launched a campaign to heighten the threat to wildlife habitats and biodiversity from plantations of fuel ...
Carbon debt and carbon sequestration parity in forest bioenergy production
The capacity for forests to aid in climate change mitigation efforts is substantial but will ultimately depend on their management. If forests remain ...
Aerosols heat up
Solid particles suspended in the atmosphere have long played second fiddle to greenhouse gases as agents of climate change. A study of atmospheric heating over ...
Climate: Sawyer predicted rate of warming in 1972
Excerpt: "In four pages Sawyer summarized what was known about the role of carbon dioxide in enhancing the natural greenhouse effect, and made a remarkable ...
A global overview of drought and heat-induced tree mortality reveals emerging climate change risks for forests
Greenhouse gas emissions have significantly altered global climate, and will continue to do so in the future. Increases in the frequency, duration, and/or ...
The State of Greenhouse Gases in the Atmosphere Based on Global Observations through 2013
The WMO Global Atmosphere Watch (GAW) coordinates observations of the most important contributors to climate change: long-lived greenhouse gases(LLGHG). In the ...
Forecasting the response of Earth’s surface to future climatic and land use changes: A review of methods and research needs
In the future, Earth will be warmer, precipitation events will be more extreme, global mean sea level will rise, and many arid and semiarid regions will be ...
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