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In Arctic landscapes, watershed processes are tightly linked to cold temperatures, permafrost, snow, and strong seasonality in precipitation, storage, and runoff. Thus, a rapidly changing Arctic climate will affect watershed function and result in changes to the transport of water, sediment, and nutrients to downstream aquatic and marine ecosystems. There is increasing evidence of hydrologic intensification of the Arctic terrestrial water cycle, fueling inquiry into the hydrologic responses that integrate the varying climate and landscape units. Key to understanding these complex watershed processes is long-term hydrologic monitoring in Arctic Alaska. The goal of this study is to operate and maintain hydroclimate observation stations in the Kuparuk River basin to obtain continuous datasets for the community of Arctic stakeholders. Imnavait Creek is a small (2.2 square kilometers) watershed located in the northern foothills region of Brooks Range and the headwaters of the Kuparuk River. The Kuparuk River flows north through the foothills and coastal plain of Alaska, before discharging into the Beaufort Sea. The gauging station at Imnavait Creek is approximately 3 kilometers south of the Dalton Highway, near MP (milepost) 291. Imnavait Creek parallels the Upper Kuparuk River and enters the Kuparuk River 12 kilometers north of the Water and Environmental Research Center (WERC) Upper Kuparuk gauging station. Streamflow at Imnavait Creek persists throughout the summer months, but during the winter months flow is non-existent. Streamflow in Imnavait Creek has been measured by researchers at the University of Alaska Fairbanks (UAF) WERC from 1985 to 2023. This data package contains continuous streamflow data collected by researchers from University of Alaska Fairbanks from 2018-2023. For UAF-WERC historical discharge data for Imnavait Creek (1985-2017) see the data package at https://arcticdata.io/catalog/view/doi%3A10.18739%2FA2K649S9D.
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Climate Change in the Lumbee River Watershed and Potential Impacts on the Lumbee Tribe of North Carolina
A growing body of research focuses on climate change and Indigenous peoples. However, relatively little of this work focuses on Native American tribes living in the Atlantic Coastal Plain of the United States. The Lumbee Tribe of North Carolina is a large (60,000 member) Native American tribe located on the Coastal Plain in present day North Carolina (U.S.). The tribe has deep connections to the Lumbee River, which flows through a watershed dominated by extensive forested wetlands. In this paper, I outline key issues associated with climate change and water in the region, and I use long‐term climatic and hydrologic datasets and analysis to establish context for understanding historical climate change in the Lumbee River watershed. Downscaled climate model outputs for the region show how further changes may affect the hydrologic balance of the watershed. I discuss these changes in terms of environmental degradation and potential impacts on Lumbee culture and persistence, which has remained strong through centuries of adversity and has also experienced a resurgence in recent years. I close by acknowledging the especially vulnerable position of the Lumbee Tribe as a non‐federal tribe that lacks access to certain resources, statutory protections, and policies aimed at helping Native American tribes deal with climate change and other environmental challenges.
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- PAR ID:
- 10058153
- Date Published:
- Journal Name:
- Journal of contemporary water research and education
- Volume:
- 163
- Issue:
- 1
- ISSN:
- 1936-704X
- Page Range / eLocation ID:
- 79-93
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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- Free Publicly Accessible Full Text
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Accepted Manuscript1.0
- Journal Article:
- https://doi.org/10.1111/j.1936-704X.2018.03271.x
