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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 ...
Adaptation: Planning for Climate Change and Its Effects on Federal Lands
National forest managers are charged with tackling the effects of climate change on the natural resources under their care. The Forest Service National ...
An Uncertain Future for Soil Carbon
Predictions of how rapidly the large amounts of carbon stored as soil organic matter will respond to warming are highly uncertain (1). Organic matter plays a ...
Emerging Techniques for Soil Carbon measurements
Soil carbon sequestration is one approach to mitigate greenhouse gases. However, to reliably assess the quantities sequestered as well as the chemical ...
Barking up the Wrong Tree? Forest Sustainability in the wake of Emerging Bioenergy Policies
The spotted owl controversy revealed that federal forest management policies alone could not guarantee functioning forest ecosystems. At the same time as the ...
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 ...
Allowable carbon emissions lowered by multiple climate targets
Climate targets are designed to inform policies that would limit the magnitude and impacts of climate change caused by anthropogenic emissions of greenhouse ...
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 ...
Controls on Annual Forest Carbon Storage: Lessons from the Past and Predictions for the Future
The temperate forests of North America may play an important role in future carbon (C) sequestration strategies. New, multiyear, ecosystem-scale C cycling ...
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 ...
Beneficial Biofuels—The Food, Energy, and Environment Trilemma
Exploiting multiple feedstocks, under new policies and accounting rules, to balance biofuel production, food security, and greenhouse-gas reduction.
Can Plants Adapt? New Questions in Climate Change Research
As it becomes increasingly apparent that human activities are partly responsible for global warming, the focus of climate change research is shifting from the ...
Growing feedback from ocean carbon to climate
The finding that feedbacks between the ocean’s carbon cycle and climate may become larger than terrestrial carbon–climate feedbacks has implications for ...
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 ...
Insect herbivory alters impact of atmospheric change on northern temperate forests
Stimulation of forest productivity by elevated concentrations of CO2 is expected to partially offset continued increases in anthropogenic CO2 emissions. ...
Tree mortality from drought, insects, and their interactions in a changing climate
Climate change is expected to drive increased tree mortality through drought, heat stress, and insect attacks, with manifold impacts on forest ecosystems. Yet, ...
Significant anthropogenic-induced changes of climate classes since 1950
Anthropogenic forcings have contributed to global and regional warming in the last few decades and likely affected terrestrial precipitation. Here we examine ...
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