Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021

Lakes are abundant features on coastal plains of the Arctic and most are termed "thermokarst" because they form in ice-rich permafrost and gradually expand over time. The dynamic nature of thermokarst lakes also makes them prone to catastrophic drainage and abrupt conversion to wetlands, c...

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Bibliographic Details
Main Author: Christopher Arp
Format: Dataset
Language:unknown
Published: Arctic Data Center 2021
Subjects:
Ice
Online Access:https://search.dataone.org/view/urn:uuid:6a4e941c-bf6c-4f63-9d0f-5bf787406729
id dataone:urn:uuid:6a4e941c-bf6c-4f63-9d0f-5bf787406729
record_format openpolar
spelling dataone:urn:uuid:6a4e941c-bf6c-4f63-9d0f-5bf787406729 2024-06-03T18:46:30+00:00 Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021 Christopher Arp Arctic Coastal Plain of northern Alaska approximately between Utqiagvik and Umiat ENVELOPE(-157.0,-150.0,72.0,69.0) BEGINDATE: 2019-05-01T00:00:00Z ENDDATE: 2021-07-12T00:00:00Z 2021-01-01T00:00:00Z https://search.dataone.org/view/urn:uuid:6a4e941c-bf6c-4f63-9d0f-5bf787406729 unknown Arctic Data Center Alaska lakes wetlands permafrost temperature hydrology Dataset 2021 dataone:urn:node:ARCTIC 2024-06-03T18:17:44Z Lakes are abundant features on coastal plains of the Arctic and most are termed "thermokarst" because they form in ice-rich permafrost and gradually expand over time. The dynamic nature of thermokarst lakes also makes them prone to catastrophic drainage and abrupt conversion to wetlands, called drained thermokarst lake basins (DTLBs). Together, thermokarst lakes and DTLBs cover up to 80% of arctic lowland regions, making understanding their response to ongoing climate change essential for coastal plain environmental assessment. Datasets presented here document water level and temperature (surface and ground) regimes for a large (38 sites) array of lake with high drainage potential and lake basin (DTLBS), which have already drained, located on differing terrain units of Alaska's Arctic Coastal Plain. Lake data was measured along deep protected shorelines using pressure transducers to record hourly water level and bed temperature. Wetland (DTLB) data was also measured with pressure transducers and ground thermistors at 25 and 100 centimeters (cm) depth. Of special interest at some DTLB sites was the potential occurrence of snow-dam outburst events during the early summer snowmelt periods. In these cases, pressure transducers were set to log at 10 minute intervals for this period. All data archived here are summarized at daily average values. Dataset Arctic Climate change Ice permafrost Thermokarst Alaska Arctic Data Center (via DataONE) Arctic ENVELOPE(-157.0,-150.0,72.0,69.0)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic Alaska
lakes
wetlands
permafrost
temperature
hydrology
spellingShingle Alaska
lakes
wetlands
permafrost
temperature
hydrology
Christopher Arp
Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021
topic_facet Alaska
lakes
wetlands
permafrost
temperature
hydrology
description Lakes are abundant features on coastal plains of the Arctic and most are termed "thermokarst" because they form in ice-rich permafrost and gradually expand over time. The dynamic nature of thermokarst lakes also makes them prone to catastrophic drainage and abrupt conversion to wetlands, called drained thermokarst lake basins (DTLBs). Together, thermokarst lakes and DTLBs cover up to 80% of arctic lowland regions, making understanding their response to ongoing climate change essential for coastal plain environmental assessment. Datasets presented here document water level and temperature (surface and ground) regimes for a large (38 sites) array of lake with high drainage potential and lake basin (DTLBS), which have already drained, located on differing terrain units of Alaska's Arctic Coastal Plain. Lake data was measured along deep protected shorelines using pressure transducers to record hourly water level and bed temperature. Wetland (DTLB) data was also measured with pressure transducers and ground thermistors at 25 and 100 centimeters (cm) depth. Of special interest at some DTLB sites was the potential occurrence of snow-dam outburst events during the early summer snowmelt periods. In these cases, pressure transducers were set to log at 10 minute intervals for this period. All data archived here are summarized at daily average values.
format Dataset
author Christopher Arp
author_facet Christopher Arp
author_sort Christopher Arp
title Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021
title_short Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021
title_full Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021
title_fullStr Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021
title_full_unstemmed Lake basin water level and ground temperature data in Arctic Alaska, 2019-2021
title_sort lake basin water level and ground temperature data in arctic alaska, 2019-2021
publisher Arctic Data Center
publishDate 2021
url https://search.dataone.org/view/urn:uuid:6a4e941c-bf6c-4f63-9d0f-5bf787406729
op_coverage Arctic Coastal Plain of northern Alaska approximately between Utqiagvik and Umiat
ENVELOPE(-157.0,-150.0,72.0,69.0)
BEGINDATE: 2019-05-01T00:00:00Z ENDDATE: 2021-07-12T00:00:00Z
long_lat ENVELOPE(-157.0,-150.0,72.0,69.0)
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Ice
permafrost
Thermokarst
Alaska
genre_facet Arctic
Climate change
Ice
permafrost
Thermokarst
Alaska
_version_ 1800867003177631744