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Highlights

Since 1989, the U.S. Global Change Research Program (USGCRP) has submitted annual reports to Congress called Our Changing Planet. The reports describe the status of USGCRP research activities, provide progress updates, and document recent accomplishments.

In particular, Our Changing Planet highlights progress and accomplishments in interagency activities. These highlights represent the broad spectrum of USGCRP activities that extend from Earth system observations, modeling, and fundamental research through synthesis and assessment, decision support, education, and public engagement.

Observations, Land Use & Land Cover, Ecosystems & Biodiversity, Arctic

Monitoring change in Alaskan forests

G-LiHT measurements for an area within Bonanza Creek Experimental Forest near Fairbanks, Alaska.

Scientists are using aerial and ground survey methods to measure change in Alaska’s interior forests and its impact on ecosystem services. 

The boreal forests of interior Alaska are changing rapidly as the climate warms. Wildfires are more frequent and more severe, and declines in growth of spruce trees may be driving a shift towards ecosystems normally found in warmer climates. These changes can have significant impacts on the quality of wildlife habitat and ecosystem services that support the subsistence economies of many native Alaskan...

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Observations, Land Use & Land Cover, Ecosystems & Biodiversity

Measuring ecosystem response to changing environments in Pacific Northwest forests

Scientists are combining satellite remote sensing and ground survey data to better understand the impacts of climate change and other disturbances on the health of Pacific Northwest forests and the ecosystem services they provide. 

Pacific Northwest forests are sensitive to temperature and drought stress and face increased vulnerability to insect pests, diseases, and fires in a changing climate. The frequency and severity of climate-related forest disturbances are expected to continue to increase over the 21st...

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Ecosystems & Biodiversity, Carbon Cycle

Understanding carbon cycling in warming northern peatlands

Figure shows how methane production changes with temperature in (a) surface and (b) deep peat samples that were anaerobically (without oxygen) incubated

Researchers are experimentally warming northern peatlands to understand carbon cycling in the climate of the future. 

Northern peatlands hold large stocks of organic carbon in their soils that are vulnerable to release into the atmosphere as the greenhouse gases carbon dioxide and methane as the climate warms. Emissions of methane, which has about 28 times the warming power...

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Ecosystems & Biodiversity, Carbon Cycle

Assessing Alaska’s carbon resources

Spatial distribution of A, annual carbon loss and gain across upland Alaska 1950–2009 and B, historical fire scars from 2000–2009 among the five Landscape Conservation Cooperative (LCC) regions.

An assessment of carbon stocks in Alaska’s soils and vegetation helped set a baseline for monitoring future change.

Alaska’s soils and vegetation store vast quantities of carbon. Increases in temperature throughout the 21st century may increasingly expose these stores to loss from increased wildfire, permafrost thaw, and other changes that could turn Alaska’s ecosystems into a net source of carbon to the atmosphere. However, much of Alaska has previously not been considered in any major national...

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Ecosystems & Biodiversity, Carbon Cycle

Predicting the future of tropical forests

A warmed TRACE plot in the USDA-Forest Service Luquillo Experimental Forest in Puerto Rico.

Field research provides new data advancing our ability to project how tropical forests will respond to a changing climate.

Tropical forests store vast amounts of carbon and play a key role in regulating Earth’s climate. As climate changes, these ecosystems have the potential to become a net contributor to global warming if they shift to releasing more carbon to the atmosphere than they absorb[1]. However, how these forests will be affected by a warming climate and changing atmosphere is still uncertain¾and is critical...

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