Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard

Abstract: Linnévatnet (78.05° N; 13.8° E; 12 m asl) is a proglacial lake located on the western coast of Spitsbergen, the largest island of the Svalbard archipelago. The 5.75 km² lake is set in a 35.3 km² catchment and fed by the glacier, Linnébreen, (1.7 km²) along with several small cirque glacier...

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Format: Dataset
Language:unknown
Published: Arctic Data Center 2013
Subjects:
Online Access:https://search.dataone.org/view/urn:uuid:e25ddc03-8644-4417-8d9c-2c6b5a993470
id dataone:urn:uuid:e25ddc03-8644-4417-8d9c-2c6b5a993470
record_format openpolar
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS
EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS
EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT
EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT
EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY
EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS
IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS
IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS
IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS
IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS
IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM
EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS
IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES
IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES
IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE
IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS
MANNED FIELD STATION
HOURLY TO DAILY
DAILY TO WEEKLY
ANNUAL
1 MINUTE TO 1 HOUR
MONTHLY TO ANNUAL
WEEKLY TO MONTHLY
spellingShingle EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS
EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS
EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT
EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT
EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY
EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS
IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS
IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS
IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS
IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS
IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM
EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS
IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES
IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES
IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE
IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS
MANNED FIELD STATION
HOURLY TO DAILY
DAILY TO WEEKLY
ANNUAL
1 MINUTE TO 1 HOUR
MONTHLY TO ANNUAL
WEEKLY TO MONTHLY
Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard
topic_facet EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS
EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS
EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS
EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT
EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT
EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY
EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS
IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS
IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS
IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS
IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS
IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM
EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS
IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES
IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES
IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE
IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS
MANNED FIELD STATION
HOURLY TO DAILY
DAILY TO WEEKLY
ANNUAL
1 MINUTE TO 1 HOUR
MONTHLY TO ANNUAL
WEEKLY TO MONTHLY
description Abstract: Linnévatnet (78.05° N; 13.8° E; 12 m asl) is a proglacial lake located on the western coast of Spitsbergen, the largest island of the Svalbard archipelago. The 5.75 km² lake is set in a 35.3 km² catchment and fed by the glacier, Linnébreen, (1.7 km²) along with several small cirque glaciers. Currently, Linnébreen covers roughly 5% of the watershed in the valley of Linnédalen. The vast majority of sediment is moved into the lake during the early summer snow melt; however, particularly warm summers increase sediment transport from the landscape into the lake as the glacier continues to generate melt-water (Werner et al., 2008; McKay, 2005). Previous sedimentological studies (Pratt, 2006; Leon, 2006; Yellen, 2006; Snyder et al., 2000) have focused on sediment cores recovered from basins proximal to the inflow delta of Linnéelva in 10 to 15 meters water depth. These studies have shown that the sediments are annually laminated (varved) in these locations. Here we present results of varve thickness measurements from two sediment cores from mooring G (B1-08, B2-08) taken in the deepest basin (35 m water depth), located in the distal northerly portion of the lake. High resolution thin section analyses down both cores find that varve thickness trends are in agreement. Increasing annual varve thickness measurements show a positive correlation (r² = 0.32, 0.18 P < 0.01) with yearly historic summer (July-August) temperature measurements from a meteorological station at Isfjord Radio Station (1947-2003 AD). External forcings (solar, volcanic, etc) appear to play a key role in environmental change, especially prior (< 1850 AD) to increased anthropogenic aerosols and CO2. Despite the relatively short length, Linnévatnet’s varve record adds to the few high-resolution climate data in a region critical for understand earth’s climate system.
format Dataset
title Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard
title_short Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard
title_full Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard
title_fullStr Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard
title_full_unstemmed Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard
title_sort pompeani 2009 a 360 year varve-based climate reconstruction from linnévatnet on western svalbard
publisher Arctic Data Center
publishDate 2013
url https://search.dataone.org/view/urn:uuid:e25ddc03-8644-4417-8d9c-2c6b5a993470
op_coverage ENVELOPE(13.731,13.896,78.066,78.028)
long_lat ENVELOPE(-26.917,-26.917,73.333,73.333)
ENVELOPE(13.933,13.933,77.967,77.967)
ENVELOPE(13.900,13.900,78.017,78.017)
ENVELOPE(13.751,13.751,78.077,78.077)
ENVELOPE(13.824,13.824,78.042,78.042)
ENVELOPE(176.683,176.683,-85.400,-85.400)
ENVELOPE(-121.386,-121.386,56.917,56.917)
ENVELOPE(13.731,13.896,78.066,78.028)
geographic Isfjord
Linnébreen
Linnédalen
Linnéelva
Linnévatnet
Pratt
Snyder
Svalbard
Svalbard Archipelago
geographic_facet Isfjord
Linnébreen
Linnédalen
Linnéelva
Linnévatnet
Pratt
Snyder
Svalbard
Svalbard Archipelago
genre glacier
Ice Sheet
Isfjord*
Isfjord*
Svalbard
Spitsbergen
genre_facet glacier
Ice Sheet
Isfjord*
Isfjord*
Svalbard
Spitsbergen
_version_ 1800872034715041792
spelling dataone:urn:uuid:e25ddc03-8644-4417-8d9c-2c6b5a993470 2024-06-03T18:46:51+00:00 Pompeani 2009 A 360 year Varve-Based Climate Reconstruction from Linnévatnet on Western Svalbard ENVELOPE(13.731,13.896,78.066,78.028) 2013-11-09T19:37:55Z https://search.dataone.org/view/urn:uuid:e25ddc03-8644-4417-8d9c-2c6b5a993470 unknown Arctic Data Center EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS MANNED FIELD STATION HOURLY TO DAILY DAILY TO WEEKLY ANNUAL 1 MINUTE TO 1 HOUR MONTHLY TO ANNUAL WEEKLY TO MONTHLY Dataset 2013 dataone:urn:node:ARCTIC 2024-06-03T18:06:29Z Abstract: Linnévatnet (78.05° N; 13.8° E; 12 m asl) is a proglacial lake located on the western coast of Spitsbergen, the largest island of the Svalbard archipelago. The 5.75 km² lake is set in a 35.3 km² catchment and fed by the glacier, Linnébreen, (1.7 km²) along with several small cirque glaciers. Currently, Linnébreen covers roughly 5% of the watershed in the valley of Linnédalen. The vast majority of sediment is moved into the lake during the early summer snow melt; however, particularly warm summers increase sediment transport from the landscape into the lake as the glacier continues to generate melt-water (Werner et al., 2008; McKay, 2005). Previous sedimentological studies (Pratt, 2006; Leon, 2006; Yellen, 2006; Snyder et al., 2000) have focused on sediment cores recovered from basins proximal to the inflow delta of Linnéelva in 10 to 15 meters water depth. These studies have shown that the sediments are annually laminated (varved) in these locations. Here we present results of varve thickness measurements from two sediment cores from mooring G (B1-08, B2-08) taken in the deepest basin (35 m water depth), located in the distal northerly portion of the lake. High resolution thin section analyses down both cores find that varve thickness trends are in agreement. Increasing annual varve thickness measurements show a positive correlation (r² = 0.32, 0.18 P < 0.01) with yearly historic summer (July-August) temperature measurements from a meteorological station at Isfjord Radio Station (1947-2003 AD). External forcings (solar, volcanic, etc) appear to play a key role in environmental change, especially prior (< 1850 AD) to increased anthropogenic aerosols and CO2. Despite the relatively short length, Linnévatnet’s varve record adds to the few high-resolution climate data in a region critical for understand earth’s climate system. Dataset glacier Ice Sheet Isfjord* Isfjord* Svalbard Spitsbergen Arctic Data Center (via DataONE) Isfjord ENVELOPE(-26.917,-26.917,73.333,73.333) Linnébreen ENVELOPE(13.933,13.933,77.967,77.967) Linnédalen ENVELOPE(13.900,13.900,78.017,78.017) Linnéelva ENVELOPE(13.751,13.751,78.077,78.077) Linnévatnet ENVELOPE(13.824,13.824,78.042,78.042) Pratt ENVELOPE(176.683,176.683,-85.400,-85.400) Snyder ENVELOPE(-121.386,-121.386,56.917,56.917) Svalbard Svalbard Archipelago ENVELOPE(13.731,13.896,78.066,78.028)