Measurements in soil and air at Samoylov Station (2002-2018) ...
Most of the world's permafrost is located in the Arctic, where its frozen organic carbon con-tent makes it a potentially important influence on the global climate system. The Arctic climate appears to be changing more rapidly than the lower latitudes, but observational data density in the regio...
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ftdatacite:10.1594/pangaea.891142 2024-03-31T07:50:57+00:00 Measurements in soil and air at Samoylov Station (2002-2018) ... Boike, Julia Nitzbon, Jan Anders, Katharina Grigoriev, Mikhail N Bolshiyanov, Dimitry Yu Langer, Moritz Lange, Stephan Bornemann, Niko Morgenstern, Anne Schreiber, Peter Wille, Christian Chadburn, Sarah Gouttevin, Isabelle Kutzbach, Lars 2018 application/zip https://dx.doi.org/10.1594/pangaea.891142 https://doi.pangaea.de/10.1594/PANGAEA.891142 en eng PANGAEA https://dx.doi.org/10.5194/essd-11-261-2019 https://dx.doi.org/10.1594/pangaea.905236 https://dx.doi.org/10.1594/pangaea.891129 https://dx.doi.org/10.1594/pangaea.891157 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Supplementary Publication Series of Datasets article Collection 2018 ftdatacite https://doi.org/10.1594/pangaea.89114210.5194/essd-11-261-201910.1594/pangaea.90523610.1594/pangaea.89112910.1594/pangaea.891157 2024-03-04T13:34:28Z Most of the world's permafrost is located in the Arctic, where its frozen organic carbon con-tent makes it a potentially important influence on the global climate system. The Arctic climate appears to be changing more rapidly than the lower latitudes, but observational data density in the region is low. Permafrost thaw and carbon release into the atmosphere is a positive feed-back mechanism that has the potential for climate warming. It is therefore particularly im-portant to understand the links between the energy balance, which can vary rapidly over hour-ly to annual time scales, and permafrost condition, which changes slowly on decadal to cen-tennial timescales. This requires long-term observational data such as that available from the Samoylov research site in northern Siberia, where meteorological parameters, energy balance, and subsurface observations have been recorded since 1998. This paper presents the temporal data set produced between 2002 and 2017, explaining the instrumentation, calibration, ... : WRONG DATA!Meteorologic data at station Samoylov (2002-2018, level 1 & level 2, version 1) are with wrong Precipitation data during the period 2009–2018.PLEASE USE NEW VERSION available at doi:10.1594/PANGAEA.905236!Precipitation was doubled during the period 2009–2018 due to incorrect application of the multiplication factor. This was due to a change in the precipitation gauge setup due to a complete destruction of the gauge sometime in autumn 2009. The broken Environmental Measurements ARG100 gauge was exchanged to an R. M. Young Company 52203 tipping bucket gauge on 26 July 2010. The required adaption of the multiplication factor (i.e. from 0.2 to 0.1) was not performed for the final calculation of the precipitation data. ... Article in Journal/Newspaper Arctic permafrost Siberia DataCite Metadata Store (German National Library of Science and Technology) Arctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
description |
Most of the world's permafrost is located in the Arctic, where its frozen organic carbon con-tent makes it a potentially important influence on the global climate system. The Arctic climate appears to be changing more rapidly than the lower latitudes, but observational data density in the region is low. Permafrost thaw and carbon release into the atmosphere is a positive feed-back mechanism that has the potential for climate warming. It is therefore particularly im-portant to understand the links between the energy balance, which can vary rapidly over hour-ly to annual time scales, and permafrost condition, which changes slowly on decadal to cen-tennial timescales. This requires long-term observational data such as that available from the Samoylov research site in northern Siberia, where meteorological parameters, energy balance, and subsurface observations have been recorded since 1998. This paper presents the temporal data set produced between 2002 and 2017, explaining the instrumentation, calibration, ... : WRONG DATA!Meteorologic data at station Samoylov (2002-2018, level 1 & level 2, version 1) are with wrong Precipitation data during the period 2009–2018.PLEASE USE NEW VERSION available at doi:10.1594/PANGAEA.905236!Precipitation was doubled during the period 2009–2018 due to incorrect application of the multiplication factor. This was due to a change in the precipitation gauge setup due to a complete destruction of the gauge sometime in autumn 2009. The broken Environmental Measurements ARG100 gauge was exchanged to an R. M. Young Company 52203 tipping bucket gauge on 26 July 2010. The required adaption of the multiplication factor (i.e. from 0.2 to 0.1) was not performed for the final calculation of the precipitation data. ... |
format |
Article in Journal/Newspaper |
author |
Boike, Julia Nitzbon, Jan Anders, Katharina Grigoriev, Mikhail N Bolshiyanov, Dimitry Yu Langer, Moritz Lange, Stephan Bornemann, Niko Morgenstern, Anne Schreiber, Peter Wille, Christian Chadburn, Sarah Gouttevin, Isabelle Kutzbach, Lars |
spellingShingle |
Boike, Julia Nitzbon, Jan Anders, Katharina Grigoriev, Mikhail N Bolshiyanov, Dimitry Yu Langer, Moritz Lange, Stephan Bornemann, Niko Morgenstern, Anne Schreiber, Peter Wille, Christian Chadburn, Sarah Gouttevin, Isabelle Kutzbach, Lars Measurements in soil and air at Samoylov Station (2002-2018) ... |
author_facet |
Boike, Julia Nitzbon, Jan Anders, Katharina Grigoriev, Mikhail N Bolshiyanov, Dimitry Yu Langer, Moritz Lange, Stephan Bornemann, Niko Morgenstern, Anne Schreiber, Peter Wille, Christian Chadburn, Sarah Gouttevin, Isabelle Kutzbach, Lars |
author_sort |
Boike, Julia |
title |
Measurements in soil and air at Samoylov Station (2002-2018) ... |
title_short |
Measurements in soil and air at Samoylov Station (2002-2018) ... |
title_full |
Measurements in soil and air at Samoylov Station (2002-2018) ... |
title_fullStr |
Measurements in soil and air at Samoylov Station (2002-2018) ... |
title_full_unstemmed |
Measurements in soil and air at Samoylov Station (2002-2018) ... |
title_sort |
measurements in soil and air at samoylov station (2002-2018) ... |
publisher |
PANGAEA |
publishDate |
2018 |
url |
https://dx.doi.org/10.1594/pangaea.891142 https://doi.pangaea.de/10.1594/PANGAEA.891142 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic permafrost Siberia |
genre_facet |
Arctic permafrost Siberia |
op_relation |
https://dx.doi.org/10.5194/essd-11-261-2019 https://dx.doi.org/10.1594/pangaea.905236 https://dx.doi.org/10.1594/pangaea.891129 https://dx.doi.org/10.1594/pangaea.891157 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.89114210.5194/essd-11-261-201910.1594/pangaea.90523610.1594/pangaea.89112910.1594/pangaea.891157 |
_version_ |
1795029439698960384 |