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Veremeeva, Alexandra; Morgenstern, Anne; Gottschalk, Milena; Jünger, Julia; Laboor, Sebastian; Abakumov, Evgeny; Adrian, Irina; Angelopoulos, Michael; Antonova, Sofia; Boike, Julia; Bornemann, Niko; Cherepanova, Alexandra; Evgrafova, Svetlana; Fedorov-Davydov, Dmitry; Fuchs, Matthias; Grigoriev, Mikhail N; Günther, Frank; Hugelius, Gustaf; Kizyakov, Alexander; Kut, Anna; Lashchinskiy, Nikolay; Lupachev, Alexey; Maksimov, Georgii T; Meyer, Hanno; Miesner, Frederieke; Minke, Merten; Nitzbon, Jan; Opel, Thomas; Overduin, Pier Paul; Ramage, Justine L; Liebner, Susanne; Polyakov, Vyacheslav I; Rivkina, Elizaveta; Runge, Alexandra; Schirrmeister, Lutz; Schwamborn, Georg; Siewert, Matthias Benjamin; Tarbeeva, Anna; Ulrich, Mathias; Wetterich, Sebastian; Zubrzycki, Sebastian; Grosse, Guido (2025): ALLena: Thaw depth measurements of the active layer in the Lena River Delta region from 1998 to 2022, Northeastern Siberia, detailed table 'Detailed_data_TD_Nitzbon' [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.983062, In: Veremeeva, A et al. (2025): ALLena: Compilation of thaw depth measurements of the active layer in the Lena River Delta region from 1998 to 2022, Northeastern Siberia [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.974408

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Published: 2025-07-01DOI registered: 2025-08-08

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Abstract:
Active layer thickness (ALT) is one of currently two Essential Climate Variables related directly to permafrost regions as defined by the Global Climate Observing System (GCOS) at the World Meteorological Organization (WMO). ALT is determined as the maximum thaw depth at the end of the thawing season and is being monitored across the Arctic to better understand climate change impacts on landscape, permafrost, hydrology, vegetation, and soil biogeochemistry. In addition, spatially and/or temporally distributed measurements of thaw depth (TD) in the active layer during the thawing period are often recorded during field work in permafrost regions for various research purposes and process understanding. The ALLena dataset presents a compilation of thaw depth (TD) measurements of the active layer in the Lena River Delta region based on published and unpublished field data collected during Russian and joint German-Russian expeditions from 1998 to 2022. The dataset contains data from different areas of the Lena Delta region with clustering in research-intensive areas, e.g. in the vicinity of Research Station Samoylov Island, but also includes sites adjacent to the delta such as Muostakh Island, Bykovsky Peninsula and Tiksi settlement surroundings. The compiled data is distributed across various ecosystems and geomorphological units underlain by different types of deposits and characterized by various relief positions, microtopography, soil and vegetation cover (e.g. active floodplains, polygonal tundra on Holocene Lena Delta terraces, remnants of Yedoma Ice Complex, etc.). TD measurements were conducted as opportunistic single as well as targeted TD transects or grid measurements. For some sites measurements of TD were repeated at the same locations in different years. TD was measured one time per site or several times per site within a few centimeters to several meters to capture small-scale heterogeneity depending on e.g. microcrotopography or vegetation type. The main datatable (doi:10.1594/PANGAEA.973813) contains discrete TD values if they were measured one to three times per site. In case of more than three TD values per measurement site, the main datatable provides the minimum, maximum, and mean TD as well as the number of measurements that were averaged. For sites with more than three TD measurements per site, separate detailed tables like this one are provided.
The dataset presents a highly valuable compilation of TD data over a uniquely large Arctic region and long time span. It might complement the Circumpolar Active Layer Monitoring (CALM) program and other published ALT and TD datasets for other permafrost regions and may be used for e.g. parametrization or validation of permafrost modelling and remote sensing studies.
Related to:
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Grigoriev, Mikhail N; Rachold, Volker; Bolshiyanov, Dimitry Yu; Pfeiffer, Eva-Maria; Schirrmeister, Lutz; Wagner, Dirk; Hubberten, Hans-Wolfgang (2003): Russian-German Cooperation System Laptev Sea 2000: The Expedition LENA 2002. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 466, 341 pp, https://doi.org/10.2312/BzPM_0466_2003
Günther, Frank; Overduin, Pier Paul; Yakshina, I A; Opel, Thomas; Baranskaya, Alisa V; Grigoriev, Mikhail N (2015): Observing Muostakh disappear: permafrost thaw subsidence and erosion of a ground-ice-rich island in response to arctic summer warming and sea ice reduction. The Cryosphere, 9(1), 151-178, https://doi.org/10.5194/tc-9-151-2015
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Kruse, Stefan; Bolshiyanov, Dimitry Yu; Grigoriev, Mikhail N; Morgenstern, Anne; Pestryakova, Luidmila A; Tsibizov, Leonid; Udke, Annegret (2019): Russian-German Cooperation: Expeditions to Siberia in 2018. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 734, 257 pp, https://doi.org/10.2312/BzPM_0734_2019
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Opel, Thomas (2015): Russian-German cooperation system Laptev Sea: The Expedition LENA 2012. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 684, 104 pp, https://doi.org/10.2312/BzPM_0684_2015
Overduin, Pier Paul; Blender, Franziska; Bolshiyanov, Dimitry Yu; Grigoriev, Mikhail N; Morgenstern, Anne; Meyer, Hanno (2017): Russian-German Cooperation: Expeditions to Siberia in 2016. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 709, 295 pp, https://doi.org/10.2312/BzPM_0709_2017
Pfeiffer, Eva-Maria; Grigoriev, Mikhail N (2002): Russian-German Cooperation System Laptev Sea 2000: The Expedition LENA 2001. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 426, 186 pp, https://doi.org/10.2312/BzPM_0426_2002
Rachold, Volker; Grigoriev, Mikhail N (1999): Russian-German Cooperation System Laptev Sea 2000: The Lena Delta 1998 Expedition. Berichte zur Polarforschung = Reports on Polar Research, 315, 1-259, https://doi.org/10.2312/BzP_0315_1_1999
Rachold, Volker; Grigoriev, Mikhail N (2000): Russian-German Cooperation System Laptev Sea 2000: The Expedition LENA 1999. Berichte zur Polarforschung = Reports on Polar Research, 354, 1-269, https://doi.org/10.2312/BzP_0354_1_2000
Rachold, Volker; Grigoriev, Mikhail N (2001): Russian-German Cooperation System Laptev Sea 2000: The Expedition LENA 2000. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 388, 135 pp, https://doi.org/10.2312/BzPM_0388_2001
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Siewert, Matthias Benjamin; Hugelius, Gustaf; Heim, Birgit; Faucherre, Samuel (2016): Landscape controls and vertical variability of soil organic carbon storage in permafrost-affected soils of the Lena River Delta. CATENA, 147, 725-741, https://doi.org/10.1016/j.catena.2016.07.048
Strauss, Jens; Boike, Julia; Bolshiyanov, Dimitry Yu; Grigoriev, Mikhail N; El-Hajj, Hassan; Morgenstern, Anne; Overduin, Pier Paul; Udke, Annegret (2018): Russian-German Cooperation: Expeditions to Siberia in 2017. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 725, 296 pp, https://doi.org/10.2312/BzPM_0725_2018
Tarbeeva, Anna; Tikhonravova, Yana; Lebedeva, Lyudmila P; Kut, Anna; Shamov, Vladimir (2024): Causes and Processes of Thermo-Erosional Gully Initiation Near Tiksi Settlement, Arctic Eastern Siberia. Permafrost and Periglacial Processes, 35(3), 357-372, https://doi.org/10.1002/ppp.2229
Ulrich, Mathias; Grosse, Guido; Chabrillat, Sabine; Schirrmeister, Lutz (2009): Spectral characterization of periglacial surfaces and geomorphological units in the Arctic Lena Delta using field spectrometry and remote sensing. Remote Sensing of Environment, 113(6), 1220-1235, https://doi.org/10.1016/j.rse.2009.02.009
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Funding:
Horizon 2020 (H2020), grant/award no. 871120: International Network for Terrestrial Research and Monitoring in the Arctic - INTERACT III
Coverage:
Median Latitude: 72.525095 * Median Longitude: 127.066485 * South-bound Latitude: 72.370300 * West-bound Longitude: 126.482900 * North-bound Latitude: 72.571534 * East-bound Longitude: 127.241560
Date/Time Start: 2017-09-10T00:00:00 * Date/Time End: 2017-09-12T00:00:00
Event(s):
Lena_TD_Sam_2017_2  * Latitude: 72.370298 * Longitude: 126.482901 * Date/Time Start: 2017-09-12T00:00:00 * Date/Time End: 2017-09-12T00:00:00 * Location: Samoylov Island (Dzhiyelyakh-Aryta Island) * Campaign: RU-Land_2017_Lena (Lena2017) * Basis: AWI Arctic Land Expedition * Method/Device: Metal probe (MPROBE)
Lena_TD_Sard_2017  * Latitude: 72.571534 * Longitude: 127.241560 * Date/Time Start: 2017-09-10T00:00:00 * Date/Time End: 2017-09-10T00:00:00 * Location: Sardakh-Sise Island * Campaign: RU-Land_2017_Lena (Lena2017) * Basis: AWI Arctic Land Expedition * Method/Device: Metal probe (MPROBE)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEventNitzbon, JanEvents contain measurements taken at one location (e. g. an island or channel) within the same year and campaign, for a specific scientific purpose, by the same PI and/or measuring person
Data IDData IDNitzbon, JanDataset ID, unique identifier for each record in this dataset (running number)
DATE/TIMEDate/TimeNitzbon, JanGeocode
LocationLocationNitzbon, Jangeneral location name of the measurement site (e. g. island or channel)
Positioning type/detailsPos typeNitzbon, Janspecifies how coordinates were obtained: handheld GPS; GNSS; map
LATITUDELatitudeNitzbon, JanGeocode – latitude of thaw depth measurement.
LONGITUDELongitudeNitzbon, JanGeocode – longitude of thaw depth measurement.
Quality flag, coordinatesQF coordNitzbon, Jan""1"" means that coordinates were not available and positions were instead identified by georeferencing of available figures. ""2"" flags coordinates that are likely wrong, because they do not match the description
Device typeDeviceNitzbon, Janmethod used to measure thaw depth: metal probe; measurement tape in soil pit; measurement tape at outcrop; measurement tape on core
10 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 1
11 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 2
12 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 3
13 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 4
14 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 5
15 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 6
16 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 7
17 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 8
18 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 9
19 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 10
20 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 11
21 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 12
22 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 13
23 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 14
24 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 15
25 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 16
26 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 17
27 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 18
28 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 19
29 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 20
30 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 21
31 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 22
32 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 23
33 Thaw depth of active layerThaw depthcmNitzbon, JanNo. 24
34 Thaw depth of active layer, meanThaw depth meancmNitzbon, Janmean of all thaw depth measurements per site
35 Thaw depth of active layer, minimumThaw depth mincmNitzbon, Janminimum of all thaw depth measurements per site. Empty if only 1 measurement was taken
36 Thaw depth of active layer, maximumThaw depth maxcmNitzbon, Janmaximum of all thaw depth measurements per site. Empty if only 1 measurement was taken
37 Method commentMethod commNitzbon, Janaveraged TD yes/no
38 Number of observationsNOBS#Nitzbon, Jannumber of thaw depth measurements per site, for which mean, max and min are provided in this row
39 MicrotopographyMicrotopoNitzbon, Jandescription of microtopography characteristics
40 GeomorphologyGeomorphologyNitzbon, Jandescription of geomorphological features
41 Publication of dataPubl dataNitzbon, Janpublication status of the thaw depth measurement data: published; unpublished
42 Data sourceData sourceNitzbon, Jansource of the thaw depth measurement data: data author/measuring person; field report; data publication
43 CampaignCampaignNitzbon, Janname of the expedition/field campaign during which the thaw depth measurements were taken
44 Data author(s)Data author(s)Nitzbon, Janperson responsible for the thaw depth measurement data
45 InstitutionInstitutionNitzbon, Janinstitute of responsible person
46 NameNameNitzbon, Janof person that conducted the thaw depth measurement in the field
47 Contact personContactNitzbon, Janname of contact person
48 CommentCommentNitzbon, Janadditional information related to the thaw depth measurement
49 Measurement typeMeasurement typeNitzbon, Janspatial type of measurements: point; transect; grid
50 Additional informationAdd infoNitzbon, JanRepeated meas: was another measurement performed at the same location at a different point in time? yes; no
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
422 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event
(Events contain measurements t...)

Data ID
(Dataset ID, unique identifier...)

Date/Time

Location
(general location name of the ...)

Pos type
(specifies how coordinates wer...)

Latitude
(latitude of thaw depth measur...)

Longitude
(longitude of thaw depth measu...)

QF coord
(""1"" means that coordinates ...)

Device
(method used to measure thaw d...)
10 
Thaw depth [cm]
(No. 1)
11 
Thaw depth [cm]
(No. 2)
12 
Thaw depth [cm]
(No. 3)
13 
Thaw depth [cm]
(No. 4)
14 
Thaw depth [cm]
(No. 5)
15 
Thaw depth [cm]
(No. 6)
16 
Thaw depth [cm]
(No. 7)
17 
Thaw depth [cm]
(No. 8)
18 
Thaw depth [cm]
(No. 9)
19 
Thaw depth [cm]
(No. 10)
20 
Thaw depth [cm]
(No. 11)
21 
Thaw depth [cm]
(No. 12)
22 
Thaw depth [cm]
(No. 13)
23 
Thaw depth [cm]
(No. 14)
24 
Thaw depth [cm]
(No. 15)
25 
Thaw depth [cm]
(No. 16)
26 
Thaw depth [cm]
(No. 17)
27 
Thaw depth [cm]
(No. 18)
28 
Thaw depth [cm]
(No. 19)
29 
Thaw depth [cm]
(No. 20)
30 
Thaw depth [cm]
(No. 21)
31 
Thaw depth [cm]
(No. 22)
32 
Thaw depth [cm]
(No. 23)
33 
Thaw depth [cm]
(No. 24)
34 
Thaw depth mean [cm]
(mean of all thaw depth measur...)
35 
Thaw depth min [cm]
(minimum of all thaw depth mea...)
36 
Thaw depth max [cm]
(maximum of all thaw depth mea...)
37 
Method comm
(averaged TD yes/no)
38 
NOBS [#]
(number of thaw depth measurem...)
39 
Microtopo
(description of microtopograph...)
40 
Geomorphology
(description of geomorphologic...)
41 
Publ data
(publication status of the tha...)
42 
Data source
(source of the thaw depth meas...)
43 
Campaign
(name of the expedition/field ...)
44 
Data author(s)
(person responsible for the th...)
45 
Institution
(institute of responsible person)
46 
Name
(of person that conducted the ...)
47 
Contact
(name of contact person)
48 
Comment
(additional information relate...)
49 
Measurement type
(spatial type of measurements:...)
50 
Add info
(Repeated meas: was another me...)
Lena_TD_Sam_2017_2 49882017-09-12Samoylov Island (Dzhiyelyakh-Aryta Island)handheld GPS72.370300126.48290metal probe35.037.039.035.034.040.036.734.040.0yes6troughunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan NitzbonMeasurements were taken during the LENA2017 land expedition to the Lena river delta on Samoylov island along a 3m long transect across a polygon rim. The measured locations are 10cm apart from each other.pointno
Lena_TD_Sam_2017_249892017-09-12Samoylov Island (Dzhiyelyakh-Aryta Island)handheld GPS72.370300126.48290metal probe45.047.051.051.053.056.055.052.051.049.051.045.056.0yes10rimunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan NitzbonMeasurements were taken during the LENA2017 land expedition to the Lena river delta on Samoylov island along a 3m long transect across a polygon rim. The measured locations are 10cm apart from each other.pointno
Lena_TD_Sam_2017_249902017-09-12Samoylov Island (Dzhiyelyakh-Aryta Island)handheld GPS72.370300126.48290metal probe47.043.043.043.041.042.043.041.046.051.057.062.067.066.049.441.067.0yes14slope to polygon centerunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan NitzbonMeasurements were taken during the LENA2017 land expedition to the Lena river delta on Samoylov island along a 3m long transect across a polygon rim. The measured locations are 10cm apart from each other.pointno
Lena_TD_Sard_2017 49912017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe42.036.036.038.031.041.021.029.038.027.037.043.031.052.040.032.045.042.042.035.033.043.041.028.036.821.052.0yes24tussock tundragentle, west facing slope towards between center and margin of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749922017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe45.047.050.044.048.047.046.844.050.0yes6wet patches and channelstransition from sloped margin towards flat center of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749932017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe34.025.024.025.026.030.022.033.027.422.034.0yes8dry patchestransition from sloped margin towards flat center of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749942017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe40.039.046.038.047.050.032.050.039.040.045.040.044.037.037.039.037.036.045.047.040.041.332.050.0yes21wet patchesflat plateau in the centre of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749952017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe30.030.033.031.039.024.025.029.033.030.025.025.030.028.029.026.032.031.028.028.033.030.025.029.324.039.0yes23dry patchesflat plateau in the centre of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749962017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe50.049.053.049.045.044.048.041.051.048.045.047.541.053.0yes11pond 1ponds in the centre of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749972017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe43.044.046.047.043.032.025.040.025.047.0yes7pond 2ponds in the centre of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749982017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe50.042.040.043.053.050.046.340.053.0yes6pond 3ponds in the centre of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201749992017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe43.044.047.044.743.047.0yes3pond 4ponds in the centre of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno
Lena_TD_Sard_201750002017-09-10Sardakh-Sise Islandhandheld GPS72.571534127.241561metal probe56.049.046.050.346.056.0yes3pond 5ponds in the centre of SardakhunpublishedData author/measuring personRU-Land_2017_LenaJulia BoikeAlfred Wegener Institute, Helmholtz Centre for Polar and Marine ResearchJan NitzbonJan Nitzbon"The ALT measurements were conducted at arbitratry (�random�) locations, and the coordinates were not recorded. The measurements were taken from the coast to the borehole in the center of the island; on the upper plateau (dry and wet patches, ponds) were taken in an 100 m radius around the borehole."pointno