Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska)

We investigated the productivity of a perennial, Arctic spring-stream. Ivishak Spring has the stable discharge (~131 L/s) and temperature (~4-8 degrees Celsius) typical for springs. It is unusual, however, in having an annual cycle of daylight from 24 hrs/d (summer) to 0 hrs/d (winter). We tested th...

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Main Author: Alexander Huryn
Format: Dataset
Language:unknown
Published: Arctic Data Center 2012
Subjects:
Online Access:https://doi.org/10.18739/A2NW7P
id dataone:doi:10.18739/A2NW7P
record_format openpolar
spelling dataone:doi:10.18739/A2NW7P 2024-06-03T18:46:34+00:00 Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska) Alexander Huryn UNITED STATES OF AMERICA > ALASKA ENVELOPE(-147.721,-147.719,69.025,69.024) BEGINDATE: 2007-03-01T00:00:00Z ENDDATE: 2009-08-31T00:00:00Z 2012-05-09T00:00:00Z https://doi.org/10.18739/A2NW7P unknown Arctic Data Center EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > SPRINGS EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > WATER TEMPERATURE EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > LAND SUBSIDENCE EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > LIGHT TRANSMISSION EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > RIVERS/STREAMS IN SITU/LABORATORY INSTRUMENTS > RADIATION SENSORS > LICOR QUANTUM SENSOR FIELD SURVEY POINT 1 MINUTE TO 1 HOUR inlandWaters Dataset 2012 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2NW7P 2024-06-03T18:08:13Z We investigated the productivity of a perennial, Arctic spring-stream. Ivishak Spring has the stable discharge (~131 L/s) and temperature (~4-8 degrees Celsius) typical for springs. It is unusual, however, in having an annual cycle of daylight from 24 hrs/d (summer) to 0 hrs/d (winter). We tested the hypothesis that stored detritus would buffer carbon limitation during winter when gross primary production (GPP) is minimized, resulting in constant rates of community respiration (CR) year-round due to constant temperatures. We used open-channel methods to measure GPP and CR monthly from March 2007 to August 2009. Mean annual GPP was 458 gC/m2. Such a level is typical for temperate desert-streams but was surprising for an Arctic stream. Annual CR (887 gC/m2) was also remarkable. The high metabolism of this stream is explained by an open canopy, moderate year round temperatures, stable bed, and high bryophyte biomass (48 gAFDM/m2). Strong seasonal cycles of GPP were mirrored by CR (r=0.65) indicating the possibility of carbon limitation during winter. This result falsified our hypothesis that CR would be relatively stable year-round due to a detritus buffer and constant temperature. README: Consult the data set README for more information about the physical location of the measurement, instrument description, data collection and processing, data remarks, and data formats. Location Information: Ivishak spring is a tributary of the Ivishak River, a braided river that flows through the Arctic National Wildlife Refuge (ANWR) on the North Slope of the Brooks Range, Alaska. Dataset Arctic Brooks Range north slope Alaska Arctic Data Center (via DataONE) Arctic Survey Point ENVELOPE(-92.082,-92.082,62.795,62.795) ENVELOPE(-147.721,-147.719,69.025,69.024)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > SPRINGS
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > WATER TEMPERATURE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > LAND SUBSIDENCE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > LIGHT TRANSMISSION
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > RIVERS/STREAMS
IN SITU/LABORATORY INSTRUMENTS > RADIATION SENSORS > LICOR QUANTUM SENSOR
FIELD SURVEY
POINT
1 MINUTE TO 1 HOUR
inlandWaters
spellingShingle EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > SPRINGS
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > WATER TEMPERATURE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > LAND SUBSIDENCE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > LIGHT TRANSMISSION
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > RIVERS/STREAMS
IN SITU/LABORATORY INSTRUMENTS > RADIATION SENSORS > LICOR QUANTUM SENSOR
FIELD SURVEY
POINT
1 MINUTE TO 1 HOUR
inlandWaters
Alexander Huryn
Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska)
topic_facet EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > SPRINGS
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > WATER TEMPERATURE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > LAND SUBSIDENCE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY > LIGHT TRANSMISSION
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > RIVERS/STREAMS
IN SITU/LABORATORY INSTRUMENTS > RADIATION SENSORS > LICOR QUANTUM SENSOR
FIELD SURVEY
POINT
1 MINUTE TO 1 HOUR
inlandWaters
description We investigated the productivity of a perennial, Arctic spring-stream. Ivishak Spring has the stable discharge (~131 L/s) and temperature (~4-8 degrees Celsius) typical for springs. It is unusual, however, in having an annual cycle of daylight from 24 hrs/d (summer) to 0 hrs/d (winter). We tested the hypothesis that stored detritus would buffer carbon limitation during winter when gross primary production (GPP) is minimized, resulting in constant rates of community respiration (CR) year-round due to constant temperatures. We used open-channel methods to measure GPP and CR monthly from March 2007 to August 2009. Mean annual GPP was 458 gC/m2. Such a level is typical for temperate desert-streams but was surprising for an Arctic stream. Annual CR (887 gC/m2) was also remarkable. The high metabolism of this stream is explained by an open canopy, moderate year round temperatures, stable bed, and high bryophyte biomass (48 gAFDM/m2). Strong seasonal cycles of GPP were mirrored by CR (r=0.65) indicating the possibility of carbon limitation during winter. This result falsified our hypothesis that CR would be relatively stable year-round due to a detritus buffer and constant temperature. README: Consult the data set README for more information about the physical location of the measurement, instrument description, data collection and processing, data remarks, and data formats. Location Information: Ivishak spring is a tributary of the Ivishak River, a braided river that flows through the Arctic National Wildlife Refuge (ANWR) on the North Slope of the Brooks Range, Alaska.
format Dataset
author Alexander Huryn
author_facet Alexander Huryn
author_sort Alexander Huryn
title Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska)
title_short Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska)
title_full Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska)
title_fullStr Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska)
title_full_unstemmed Ecosystem metabolism for an arctic warm spring-stream (Ivishak Hot Spring, Alaska)
title_sort ecosystem metabolism for an arctic warm spring-stream (ivishak hot spring, alaska)
publisher Arctic Data Center
publishDate 2012
url https://doi.org/10.18739/A2NW7P
op_coverage UNITED STATES OF AMERICA > ALASKA
ENVELOPE(-147.721,-147.719,69.025,69.024)
BEGINDATE: 2007-03-01T00:00:00Z ENDDATE: 2009-08-31T00:00:00Z
long_lat ENVELOPE(-92.082,-92.082,62.795,62.795)
ENVELOPE(-147.721,-147.719,69.025,69.024)
geographic Arctic
Survey Point
geographic_facet Arctic
Survey Point
genre Arctic
Brooks Range
north slope
Alaska
genre_facet Arctic
Brooks Range
north slope
Alaska
op_doi https://doi.org/10.18739/A2NW7P
_version_ 1800867927307583488