Water balance measurements on Samoylov Island during campaign Lena2011 ...

The summer water balance of a typical Siberian polygonal tundra catchment is investigated in order to identify the spatial and temporal dynamics of its main hydrological processes. The results show that, besides precipitation and evapotranspiration, lateral flow considerably influences the site-spec...

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Main Authors: Helbig, Manuel, Boike, Julia, Langer, Moritz, Schreiber, Peter, Runkle, Benjamin R K, Kutzbach, Lars
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.811079
https://doi.pangaea.de/10.1594/PANGAEA.811079
id ftdatacite:10.1594/pangaea.811079
record_format openpolar
spelling ftdatacite:10.1594/pangaea.811079 2024-09-15T18:17:44+00:00 Water balance measurements on Samoylov Island during campaign Lena2011 ... Helbig, Manuel Boike, Julia Langer, Moritz Schreiber, Peter Runkle, Benjamin R K Kutzbach, Lars 2013 application/zip https://dx.doi.org/10.1594/pangaea.811079 https://doi.pangaea.de/10.1594/PANGAEA.811079 en eng PANGAEA https://dx.doi.org/10.1007/s10040-012-0933-4 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Arctic Tundra Evaporation hydraulic conductivity island precipitation article Collection Supplementary Publication Series of Datasets 2013 ftdatacite https://doi.org/10.1594/pangaea.81107910.1007/s10040-012-0933-4 2024-08-01T11:01:35Z The summer water balance of a typical Siberian polygonal tundra catchment is investigated in order to identify the spatial and temporal dynamics of its main hydrological processes. The results show that, besides precipitation and evapotranspiration, lateral flow considerably influences the site-specific hydrological conditions. The prominent microtopography of the polygonal tundra strongly controls lateral flow and storage behaviour of the investigated catchment. Intact rims of low-centred polygons build hydrological barriers, which release storage water later in summer than polygons with degraded rims and troughs above degraded ice wedges. The barrier function of rims is strongly controlled by soil thaw, which opens new subsurface flow paths and increases subsurface hydrological connectivity. Therefore, soil thaw dynamics determine the magnitude and timing of subsurface outflow and the redistribution of storage within the catchment. Hydraulic conductivities in the elevated polygonal rims sharply decrease ... : Supplement to: Helbig, Manuel; Boike, Julia; Langer, Moritz; Schreiber, Peter; Runkle, Benjamin R K; Kutzbach, Lars (2013): Spatial and seasonal variability of polygonal tundra water balance: Lena River Delta, northern Siberia (Russia). Hydrogeology Journal, 21(1), 133-147 ... Article in Journal/Newspaper lena river Tundra Siberia DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Arctic Tundra
Evaporation
hydraulic conductivity
island
precipitation
spellingShingle Arctic Tundra
Evaporation
hydraulic conductivity
island
precipitation
Helbig, Manuel
Boike, Julia
Langer, Moritz
Schreiber, Peter
Runkle, Benjamin R K
Kutzbach, Lars
Water balance measurements on Samoylov Island during campaign Lena2011 ...
topic_facet Arctic Tundra
Evaporation
hydraulic conductivity
island
precipitation
description The summer water balance of a typical Siberian polygonal tundra catchment is investigated in order to identify the spatial and temporal dynamics of its main hydrological processes. The results show that, besides precipitation and evapotranspiration, lateral flow considerably influences the site-specific hydrological conditions. The prominent microtopography of the polygonal tundra strongly controls lateral flow and storage behaviour of the investigated catchment. Intact rims of low-centred polygons build hydrological barriers, which release storage water later in summer than polygons with degraded rims and troughs above degraded ice wedges. The barrier function of rims is strongly controlled by soil thaw, which opens new subsurface flow paths and increases subsurface hydrological connectivity. Therefore, soil thaw dynamics determine the magnitude and timing of subsurface outflow and the redistribution of storage within the catchment. Hydraulic conductivities in the elevated polygonal rims sharply decrease ... : Supplement to: Helbig, Manuel; Boike, Julia; Langer, Moritz; Schreiber, Peter; Runkle, Benjamin R K; Kutzbach, Lars (2013): Spatial and seasonal variability of polygonal tundra water balance: Lena River Delta, northern Siberia (Russia). Hydrogeology Journal, 21(1), 133-147 ...
format Article in Journal/Newspaper
author Helbig, Manuel
Boike, Julia
Langer, Moritz
Schreiber, Peter
Runkle, Benjamin R K
Kutzbach, Lars
author_facet Helbig, Manuel
Boike, Julia
Langer, Moritz
Schreiber, Peter
Runkle, Benjamin R K
Kutzbach, Lars
author_sort Helbig, Manuel
title Water balance measurements on Samoylov Island during campaign Lena2011 ...
title_short Water balance measurements on Samoylov Island during campaign Lena2011 ...
title_full Water balance measurements on Samoylov Island during campaign Lena2011 ...
title_fullStr Water balance measurements on Samoylov Island during campaign Lena2011 ...
title_full_unstemmed Water balance measurements on Samoylov Island during campaign Lena2011 ...
title_sort water balance measurements on samoylov island during campaign lena2011 ...
publisher PANGAEA
publishDate 2013
url https://dx.doi.org/10.1594/pangaea.811079
https://doi.pangaea.de/10.1594/PANGAEA.811079
genre lena river
Tundra
Siberia
genre_facet lena river
Tundra
Siberia
op_relation https://dx.doi.org/10.1007/s10040-012-0933-4
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.81107910.1007/s10040-012-0933-4
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