Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016

The dataset contains subsurface temperature measurements done at Lomonosovfonna, Svalbard, during April 2012 - 2016. All measurements are done at the site with coordinates: 78.8235 N, 17.432 E. The data is contained in four cells of a matlab structure containing data from installations deployed in A...

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Bibliographic Details
Main Authors: Marchenko, Sergey, Pohjola, Veijo A, Pettersson, Rickard
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
TP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.902613
https://doi.org/10.1594/PANGAEA.902613
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.902613
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic firn
Lomonosovfonna
Lomonosovfonna_subT
snow
Svalbard
Norway
Temperature
Temperature probe
TP
spellingShingle firn
Lomonosovfonna
Lomonosovfonna_subT
snow
Svalbard
Norway
Temperature
Temperature probe
TP
Marchenko, Sergey
Pohjola, Veijo A
Pettersson, Rickard
Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016
topic_facet firn
Lomonosovfonna
Lomonosovfonna_subT
snow
Svalbard
Norway
Temperature
Temperature probe
TP
description The dataset contains subsurface temperature measurements done at Lomonosovfonna, Svalbard, during April 2012 - 2016. All measurements are done at the site with coordinates: 78.8235 N, 17.432 E. The data is contained in four cells of a matlab structure containing data from installations deployed in April 2012 - cell 1, April 2013 - cell 2, April 2014 - cell 3 and April 2015 - cell 4. In 2012-2014 nine thermistor strings were installed in each year. The nine T-strings were arranged in a 3*3 square grid with a 3 m spacing between neighboring strings. In 2015 one t-string was installed. Hardware: Campbell Scientific CR10X data loggers in combination with several relay multiplexers (AM416 of AM16/32B) were used for temperature measurements. For that a reference temperature stable resistor (Rr Ohm) was connected is series with thermistors. Known excitation voltage (Ue) was supplied to the circuit and the voltage was measured (Um) at the leads of the reference resistor. The resistance of a thermistor (Rt) was then calculated as: Rt = Ue * Rr / Um - Rr. The resistance was then converted to temperature values provided by the manufacturer of thermistors. Technical information is contained in the variables: LF{N}.T.system. The raw temperature measurements along with the time stamps and depths are contained in the variables LF{N}.T.system.T_raw, LF{N}.T.system.t_raw and LF{N}.T.system.z_raw. After unpacking the data was subjected to the following post-processing steps: - delete data from sensors that were left above the snow surface - for the sensors installed in April 2013: delete data after 2013 July 12 - reset temperature values outsides of the range [-40 +10] degC to NaN - for the sensors installed in April 2015: correct values from one of the sensors by linear interpolation in time between the following time points: 2015 November 15 02:00 and 2015 November 15 14:00, 2015 December 18 15:00 and 2015 December 19 21:00 - introduce corrections to depths of sensors to match temperature distributions measured at different ...
format Dataset
author Marchenko, Sergey
Pohjola, Veijo A
Pettersson, Rickard
author_facet Marchenko, Sergey
Pohjola, Veijo A
Pettersson, Rickard
author_sort Marchenko, Sergey
title Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016
title_short Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016
title_full Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016
title_fullStr Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016
title_full_unstemmed Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016
title_sort subsurface temperature at lomonosovfonna, svalbard, april 2012-2016
publisher PANGAEA
publishDate 2019
url https://doi.pangaea.de/10.1594/PANGAEA.902613
https://doi.org/10.1594/PANGAEA.902613
op_coverage LATITUDE: 78.823500 * LONGITUDE: 17.432000
long_lat ENVELOPE(17.663,17.663,78.774,78.774)
ENVELOPE(17.432000,17.432000,78.823500,78.823500)
geographic Svalbard
Norway
Lomonosovfonna
geographic_facet Svalbard
Norway
Lomonosovfonna
genre Journal of Glaciology
Svalbard
The Cryosphere
genre_facet Journal of Glaciology
Svalbard
The Cryosphere
op_relation Marchenko, Sergey; Cheng, Gong; Lötstedt, Per; Pohjola, Veijo A; Pettersson, Rickard; van Pelt, Ward; Reijmer, Carleen H (2019): Thermal conductivity of firn at Lomonosovfonna, Svalbard, derived from subsurface temperature measurements. The Cryosphere, 13(7), 1843-1859, https://doi.org/10.5194/tc-13-1843-2019
Marchenko, Sergey; Pohjola, Veijo A; Pettersson, Rickard; van Pelt, Ward; Vega, Carmen Paulina; Machguth, Horst; Bøggild, Carl E; Isaksson, Elisabeth (2017): A plot-scale study of firn stratigraphy at Lomonosovfonna, Svalbard, using ice cores, borehole video and GPR surveys in 2012–14. Journal of Glaciology, 63(237), 67-78, https://doi.org/10.1017/jog.2016.118
Marchenko, Sergey; van Pelt, Ward; Claremar, Björn; Pohjola, Veijo A; Pettersson, Rickard; Machguth, Horst; Reijmer, Carleen H (2017): Parameterizing Deep Water Percolation Improves Subsurface Temperature Simulations by a Multilayer Firn Model. Frontiers in Earth Science, 5, https://doi.org/10.3389/feart.2017.00016
https://doi.pangaea.de/10.1594/PANGAEA.902613
https://doi.org/10.1594/PANGAEA.902613
op_rights CC-BY-ND-4.0: Creative Commons Attribution-NoDerivs 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY-ND
op_doi https://doi.org/10.1594/PANGAEA.902613
https://doi.org/10.5194/tc-13-1843-2019
https://doi.org/10.1017/jog.2016.118
https://doi.org/10.3389/feart.2017.00016
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spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.902613 2023-05-15T16:57:39+02:00 Subsurface temperature at Lomonosovfonna, Svalbard, April 2012-2016 Marchenko, Sergey Pohjola, Veijo A Pettersson, Rickard LATITUDE: 78.823500 * LONGITUDE: 17.432000 2019-06-13 application/zip, 42.1 MBytes https://doi.pangaea.de/10.1594/PANGAEA.902613 https://doi.org/10.1594/PANGAEA.902613 en eng PANGAEA Marchenko, Sergey; Cheng, Gong; Lötstedt, Per; Pohjola, Veijo A; Pettersson, Rickard; van Pelt, Ward; Reijmer, Carleen H (2019): Thermal conductivity of firn at Lomonosovfonna, Svalbard, derived from subsurface temperature measurements. The Cryosphere, 13(7), 1843-1859, https://doi.org/10.5194/tc-13-1843-2019 Marchenko, Sergey; Pohjola, Veijo A; Pettersson, Rickard; van Pelt, Ward; Vega, Carmen Paulina; Machguth, Horst; Bøggild, Carl E; Isaksson, Elisabeth (2017): A plot-scale study of firn stratigraphy at Lomonosovfonna, Svalbard, using ice cores, borehole video and GPR surveys in 2012–14. Journal of Glaciology, 63(237), 67-78, https://doi.org/10.1017/jog.2016.118 Marchenko, Sergey; van Pelt, Ward; Claremar, Björn; Pohjola, Veijo A; Pettersson, Rickard; Machguth, Horst; Reijmer, Carleen H (2017): Parameterizing Deep Water Percolation Improves Subsurface Temperature Simulations by a Multilayer Firn Model. Frontiers in Earth Science, 5, https://doi.org/10.3389/feart.2017.00016 https://doi.pangaea.de/10.1594/PANGAEA.902613 https://doi.org/10.1594/PANGAEA.902613 CC-BY-ND-4.0: Creative Commons Attribution-NoDerivs 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY-ND firn Lomonosovfonna Lomonosovfonna_subT snow Svalbard Norway Temperature Temperature probe TP Dataset 2019 ftpangaea https://doi.org/10.1594/PANGAEA.902613 https://doi.org/10.5194/tc-13-1843-2019 https://doi.org/10.1017/jog.2016.118 https://doi.org/10.3389/feart.2017.00016 2023-01-20T09:12:28Z The dataset contains subsurface temperature measurements done at Lomonosovfonna, Svalbard, during April 2012 - 2016. All measurements are done at the site with coordinates: 78.8235 N, 17.432 E. The data is contained in four cells of a matlab structure containing data from installations deployed in April 2012 - cell 1, April 2013 - cell 2, April 2014 - cell 3 and April 2015 - cell 4. In 2012-2014 nine thermistor strings were installed in each year. The nine T-strings were arranged in a 3*3 square grid with a 3 m spacing between neighboring strings. In 2015 one t-string was installed. Hardware: Campbell Scientific CR10X data loggers in combination with several relay multiplexers (AM416 of AM16/32B) were used for temperature measurements. For that a reference temperature stable resistor (Rr Ohm) was connected is series with thermistors. Known excitation voltage (Ue) was supplied to the circuit and the voltage was measured (Um) at the leads of the reference resistor. The resistance of a thermistor (Rt) was then calculated as: Rt = Ue * Rr / Um - Rr. The resistance was then converted to temperature values provided by the manufacturer of thermistors. Technical information is contained in the variables: LF{N}.T.system. The raw temperature measurements along with the time stamps and depths are contained in the variables LF{N}.T.system.T_raw, LF{N}.T.system.t_raw and LF{N}.T.system.z_raw. After unpacking the data was subjected to the following post-processing steps: - delete data from sensors that were left above the snow surface - for the sensors installed in April 2013: delete data after 2013 July 12 - reset temperature values outsides of the range [-40 +10] degC to NaN - for the sensors installed in April 2015: correct values from one of the sensors by linear interpolation in time between the following time points: 2015 November 15 02:00 and 2015 November 15 14:00, 2015 December 18 15:00 and 2015 December 19 21:00 - introduce corrections to depths of sensors to match temperature distributions measured at different ... Dataset Journal of Glaciology Svalbard The Cryosphere PANGAEA - Data Publisher for Earth & Environmental Science Svalbard Norway Lomonosovfonna ENVELOPE(17.663,17.663,78.774,78.774) ENVELOPE(17.432000,17.432000,78.823500,78.823500)