The Arctic is warming at higher rates than much of the rest of the world. For Alaska, this results in changes in hydrology and ecosystems – permafrost is thawing, changing landscapes and releasing nutrients to soils and streams.
Return to Water or Landscape Science >> Arctic – Boreal Catchment Studies
The Arctic is warming at higher rates than much of the rest of the world. For Alaska, this results in changes in hydrology and ecosystems – permafrost is thawing, changing landscapes and releasing nutrients to soils and streams. Landscapes and streams are warming, affecting plant growth and fish and wildlife habitat. HEAT aims to understand the impacts of warming on the ecosystems at the Arctic-boreal transition, in the Noatak Preserve in northwestern Alaska. Here, catchments are near the physiographic limit of where trees can grow, and thus vegetation is dominated either by tundra or forest, depending on aspect and elevation. These different land cover types impact water storage, and the movement of water and nutrients from the catchments to the streams. By considering differences in temperatures, stream inflows, biogeochemical cycling, and fish presence, growth, and movement, this project aims to understand the link between physical changes in stream chemistry and fish ecology, with an eye towards how these links will change in the future.
This product is in conjuction with Hydro-ecology of Arctic Thawing (HEAT): Ecology
Below are other science projects associated with this project.
Arctic – Boreal Catchment Studies
Below are data or web applications associated with this project.
Water Level, Temperature, and Discharge of Headwater Streams in the Noatak and Kobuk River Basins, Northwest Alaska, 2015-2017 Water Level, Temperature, and Discharge of Headwater Streams in the Noatak and Kobuk River Basins, Northwest Alaska, 2015-2017
Below are multimedia items associated with this project.
Below are publications associated with this project.
Below are news stories associated with this project.
The Arctic is warming at higher rates than much of the rest of the world. For Alaska, this results in changes in hydrology and ecosystems – permafrost is thawing, changing landscapes and releasing nutrients to soils and streams.
Return to Water or Landscape Science >> Arctic – Boreal Catchment Studies
The Arctic is warming at higher rates than much of the rest of the world. For Alaska, this results in changes in hydrology and ecosystems – permafrost is thawing, changing landscapes and releasing nutrients to soils and streams. Landscapes and streams are warming, affecting plant growth and fish and wildlife habitat. HEAT aims to understand the impacts of warming on the ecosystems at the Arctic-boreal transition, in the Noatak Preserve in northwestern Alaska. Here, catchments are near the physiographic limit of where trees can grow, and thus vegetation is dominated either by tundra or forest, depending on aspect and elevation. These different land cover types impact water storage, and the movement of water and nutrients from the catchments to the streams. By considering differences in temperatures, stream inflows, biogeochemical cycling, and fish presence, growth, and movement, this project aims to understand the link between physical changes in stream chemistry and fish ecology, with an eye towards how these links will change in the future.
This product is in conjuction with Hydro-ecology of Arctic Thawing (HEAT): Ecology
Below are other science projects associated with this project.
Arctic – Boreal Catchment Studies
Below are data or web applications associated with this project.
Water Level, Temperature, and Discharge of Headwater Streams in the Noatak and Kobuk River Basins, Northwest Alaska, 2015-2017 Water Level, Temperature, and Discharge of Headwater Streams in the Noatak and Kobuk River Basins, Northwest Alaska, 2015-2017
Below are multimedia items associated with this project.
Below are publications associated with this project.
Below are news stories associated with this project.