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Ecosystems Land Change Science Program

The Land Change Science Program in the USGS Ecosystems Mission Area strives to advance the understanding of the physical, chemical, and biological components of the Earth system, the causes and consequences of ecosystem and land use change, and the vulnerability and resilience of the Earth system to such changes.

News

New tree-ring science demonstrates successful restoration of historical fire patterns in two southwestern wilderness areas

New tree-ring science demonstrates successful restoration of historical fire patterns in two southwestern wilderness areas

EcoNews | Winter 2026 - Vol. 7 | Issue 1

EcoNews | Winter 2026 - Vol. 7 | Issue 1

Earth Science Matters - Vol. 21 | Issue 1

Earth Science Matters - Vol. 21 | Issue 1

Publications

Representing 3-dimensional fuels for physics-based fire behavior models: A general framework and case study in a type-converted post-fire shrubfield Representing 3-dimensional fuels for physics-based fire behavior models: A general framework and case study in a type-converted post-fire shrubfield

Background Physics-based three-dimensional (3D) fire behavior models improve planning for prescribed fire application and wildfire mitigation, but require high spatial resolution 3D fuel models as inputs. While multiple methods and data sources for realistically representing 3D, heterogeneous fuels are available, no unifying framework exists to guide the use of these tools to create 3D...
Authors
Niko Tutland, Andreas Paul Wion, Carolina Jasmine May, Grant C. Hutchings, Hope Nowak, James R. Gattiker, J. Kevin Hiers, Rodman R. Linn, Scott M. Pokswinski, Ellis Q. Margolis

Linking fire radiative power to land cover, fire history, and environmental setting in Alaska, 2003–2022 Linking fire radiative power to land cover, fire history, and environmental setting in Alaska, 2003–2022

Background Fire radiative power (FRP) shows promise as a diagnostic and predictive indicator of fire behavior and post-fire effects in Alaska, USA. Aims To investigate relationships between FRP, vegetation functional groups, and environmental settings in Alaska (2003–2022) under various fire history conditions. Methods We tested for distinctness of MODIS FRP distributions associated with...
Authors
Jessica J. Walker, Rachel A. Loehman, Britt Windsor Smith, Christopher E. Soulard

An early Holocene wet period in the southwestern United States An early Holocene wet period in the southwestern United States

Multiple generations of spring-fed streams traversed ∼800 km2 of the Las Vegas Valley in southern Nevada between ca. 10.9 ka and 8.5 ka, depositing an extensive tufa network. The scale of this network and diversity of tufa morphologies is novel in North America and offers an opportunity to obtain quantitative paleoclimate data for the region during the early Holocene. We determined...
Authors
Kathleen B. Springer, Adam M. Hudson, Jeffrey S. Pigati, Katharine W. Huntington, Andrew J. Schauer

Science

Wolverine Glacier

Wolverine Glacier is located in the high-latitude maritime climate regime of Alaska’s Kenai Mountains. Glacier observations began at this site in 1966.
Wolverine Glacier

Wolverine Glacier

Wolverine Glacier is located in the high-latitude maritime climate regime of Alaska’s Kenai Mountains. Glacier observations began at this site in 1966.
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Lemon Creek Glacier

Lemon Creek Glacier is located in the high-latitude maritime region of Alaska, at the southernmost tip of the Juneau Icefield. Glacier observations began at this site in 1953.
Lemon Creek Glacier

Lemon Creek Glacier

Lemon Creek Glacier is located in the high-latitude maritime region of Alaska, at the southernmost tip of the Juneau Icefield. Glacier observations began at this site in 1953.
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Gulkana Glacier

Gulkana Glacier is located in the high-latitude continental climate regime of Alaska’s Delta Mountains. Glacier observations began at this site in 1966.
Gulkana Glacier

Gulkana Glacier

Gulkana Glacier is located in the high-latitude continental climate regime of Alaska’s Delta Mountains. Glacier observations began at this site in 1966.
Learn More
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