Baseline characteristics of climate, permafrost, and land cover from Samoylov Island, Lena River Delta, Siberia

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Hauptverfasser: Boike, Julia, Kattenstroth, Britta, Abramova, Katya, Bornemann, Niko, Chetverova, Antonina, Fedorova, Irina V, Fröb, Katrin, Grigoriev, Mikhail N, Grüber, Maren, Kutzbach, Lars, Langer, Moritz, Minke, Merten, Muster, Sina, Piel, Konstanze, Pfeiffer, Eva-Maria, Stoof, Günter, Westermann, Sebastian, Wischnewski, Karoline, Wille, Christian, Hubberten, Hans-Wolfgang
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2013
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author Boike, Julia
Kattenstroth, Britta
Abramova, Katya
Bornemann, Niko
Chetverova, Antonina
Fedorova, Irina V
Fröb, Katrin
Grigoriev, Mikhail N
Grüber, Maren
Kutzbach, Lars
Langer, Moritz
Minke, Merten
Muster, Sina
Piel, Konstanze
Pfeiffer, Eva-Maria
Stoof, Günter
Westermann, Sebastian
Wischnewski, Karoline
Wille, Christian
Hubberten, Hans-Wolfgang
author_facet Boike, Julia
Kattenstroth, Britta
Abramova, Katya
Bornemann, Niko
Chetverova, Antonina
Fedorova, Irina V
Fröb, Katrin
Grigoriev, Mikhail N
Grüber, Maren
Kutzbach, Lars
Langer, Moritz
Minke, Merten
Muster, Sina
Piel, Konstanze
Pfeiffer, Eva-Maria
Stoof, Günter
Westermann, Sebastian
Wischnewski, Karoline
Wille, Christian
Hubberten, Hans-Wolfgang
collection Datos científicos de ciencias marinas y ambientales
contents Samoylov Island is centrally located within the Lena River Delta at 72° N, 126° E and lies within the Siberian zone of continuous permafrost. The landscape on Samoylov Island consists mainly of late Holocene river terraces with polygonal tundra, ponds and lakes, and an active floodplain. The island has been the focus of numerous multidisciplinary studies since 1993, which have focused on climate, land cover, ecology, hydrology, permafrost and limnology. This paper aims to provide a framework for future studies by describing the characteristics of the island's meteorological parameters (temperature, radiation and snow cover), soil temperature, and soil moisture. The land surface characteristics have been described using high resolution aerial images in combination with data from ground-based observations. Of note is that deeper permafrost temperatures have increased between 0.3 to 1.3 °C over the last five years. However, no clear warming of air and active layer temperatures is detected since 1998, though winter air temperatures during recent years have not been as cold as in earlier years.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_806233
institution PANGAEA
language en
publishDate 2013
publisher PANGAEA
record_format pangaea
spellingShingle Baseline characteristics of climate, permafrost, and land cover from Samoylov Island, Lena River Delta, Siberia
Boike, Julia
Kattenstroth, Britta
Abramova, Katya
Bornemann, Niko
Chetverova, Antonina
Fedorova, Irina V
Fröb, Katrin
Grigoriev, Mikhail N
Grüber, Maren
Kutzbach, Lars
Langer, Moritz
Minke, Merten
Muster, Sina
Piel, Konstanze
Pfeiffer, Eva-Maria
Stoof, Günter
Westermann, Sebastian
Wischnewski, Karoline
Wille, Christian
Hubberten, Hans-Wolfgang
AWI_PerDyn; Changing Permafrost in the Arctic and its Global Effects in the 21st Century; Evaporation; Lake/Pond; PAGE21; Permafrost Research (Periglacial Dynamics) @ AWI; precipitation; snow density; soil temperature; Water temperature; wind speed
Samoylov Island is centrally located within the Lena River Delta at 72° N, 126° E and lies within the Siberian zone of continuous permafrost. The landscape on Samoylov Island consists mainly of late Holocene river terraces with polygonal tundra, ponds and lakes, and an active floodplain. The island has been the focus of numerous multidisciplinary studies since 1993, which have focused on climate, land cover, ecology, hydrology, permafrost and limnology. This paper aims to provide a framework for future studies by describing the characteristics of the island's meteorological parameters (temperature, radiation and snow cover), soil temperature, and soil moisture. The land surface characteristics have been described using high resolution aerial images in combination with data from ground-based observations. Of note is that deeper permafrost temperatures have increased between 0.3 to 1.3 °C over the last five years. However, no clear warming of air and active layer temperatures is detected since 1998, though winter air temperatures during recent years have not been as cold as in earlier years.
title Baseline characteristics of climate, permafrost, and land cover from Samoylov Island, Lena River Delta, Siberia
topic AWI_PerDyn; Changing Permafrost in the Arctic and its Global Effects in the 21st Century; Evaporation; Lake/Pond; PAGE21; Permafrost Research (Periglacial Dynamics) @ AWI; precipitation; snow density; soil temperature; Water temperature; wind speed
url https://doi.org/10.1594/PANGAEA.806233