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...
Main Authors: | , , , , , |
---|---|
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 |
_version_ |
1810455826017550336 |