This project is part of Navigating the New Arctic (NNA) which addresses converging scientific challenges in the rapidly changing Arctic. Specifically, the goal of this project is to better understand ice-rich permafrost at local, regional, and circumpolar scales. This dataset provides ground temperature data in the active layer and near-surface permafrost to provide a baseline for assessing the future changes in the near-surface temperatures in the natural environment and next to the infrastructure/disturbed environment at Utqiagvik, Alaska. Collected ground temperature data are intended to help researchers, communities and public with ongoing activities to mitigate a threat of thawing permafrost on the local and regional scale, and to provide spatial data for validation of climate scenario models and temperature reanalysis approaches.
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A new ice-rich-permafrost-system observatory, Prudhoe Bay Oilfield, Alaska: landscape evolution on ice-rich calcareous fluvial, eolian, and lacustrine deposits
Long-term permafrost observatories are needed to document and monitor rapid changes to ice-rich permafrost systems (IRPS) in a variety of geological, climatic, and infrastructure settings. As part of the US National Science Foundation’s Navigating the New Arctic (NNA) Program, a new observatory was established near the Deadhorse Airport in the eastern part of the Prudhoe Bay Oilfield (PBO) in 2020–23. The NNA-IRPS project has three main research themes: (1) evolution of and degradation of ground ice within the major surficial-geology units; (2) rapid changes in permafrost, landforms, and vegetation due to infrastructure and climate change; and (3) ecological landscapes associated with the calcareous fluvial deposits of the Central Arctic Coastal Plain.
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- Award ID(s):
- 1928237
- PAR ID:
- 10537683
- Publisher / Repository:
- NSF PAR
- Date Published:
- Subject(s) / Keyword(s):
- ice-rich permafrost permafrost degradation arctic prudhoe bay landscape evolution tundra vegetation observatory
- Format(s):
- Medium: X
- Location:
- Whitehorse, Yukon, Canada
- Sponsoring Org:
- National Science Foundation
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This project is part of Navigating the New Arctic (NNA) which addresses converging scientific challenges in the rapidly changing Arctic. Specifically, the goal of this project is to better understand ice-rich permafrost at local, regional, and circumpolar scales. This dataset provides ground temperature data in the active layer and near-surface permafrost to provide a baseline for assessing the future changes in the near-surface temperatures in the natural environment and next to the infrastructure/disturbed environment at Utqiagvik, Point Lay, and Wainwright in Alaska. Collected ground temperature data are intended to help researchers, communities and public with ongoing activities to mitigate a threat of thawing permafrost on the local and regional scale, and to provide spatial data for validation of climate scenario models and temperature reanalysis approaches. Update: Filename nomenclature has been changed from US_PIP_### to US_UTQ_### in order to separate different site location data.more » « less
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Abstract. Rapid Arctic climate warming, amplified relative to lower-latitude regions, has led to permafrost thaw and associated thermokarst processes. Recent work has shown permafrost is a rich source of ice-nucleating particles (INPs) that can initiate ice formation in supercooled liquid clouds. Since the phase of Arctic clouds strongly affects the surface energy budget, especially over ice-laden surfaces, characterizing INP sources in this region is critical. For the first time, we provide a large-scale survey of potential INP sources in tundra terrain where thermokarst processes are active and relate to INPs in the air. Permafrost, seasonally thawed active layer, ice wedge, vegetation, water, and aerosol samples were collected near Utqiaġvik, Alaska, in late summer and analyzed for their INP contents. Permafrost was confirmed as a rich source of INPs that was enhanced near the coast. Sensitivity to heating revealed differences in INPs from similar sources, such as the permafrost and active layer. Water, vegetation, and ice wedge INPs had the highest heat-labile percentage. The aerosol likely contained a mixture of known and unsurveyed INP types that were inferred as biological. Arctic water bodies were shown to be potential important links of sources to the atmosphere in thermokarst regions. Therefore, a positive relationship found with total organic carbon considering all water bodies gives a mechanism for future parameterization as permafrost continues to thaw and drive regional landscape shifts.more » « less
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