The water temperature characteristics of the Lena River at basin outlet in the summer period

The water temperature characteristics of the Lena River at basin outlet during the summer season (June–September) are considered. The analysis is based on a long-term data series covering the period from the beginning of observation (1936) to the present time (2012) at Kusur (Kyusyur) gauging statio...

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Main Authors: Fofonova, Vera, Zhilyaev, Igor, Krayneva, Marina, Yakshina, Dina, Tananaev, Nikita, Volkova, Nina, Wiltshire, Karen H.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/hess-2016-254
https://www.hydrol-earth-syst-sci-discuss.net/hess-2016-254/
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spelling ftcopernicus:oai:publications.copernicus.org:hessd51516 2023-05-15T17:07:36+02:00 The water temperature characteristics of the Lena River at basin outlet in the summer period Fofonova, Vera Zhilyaev, Igor Krayneva, Marina Yakshina, Dina Tananaev, Nikita Volkova, Nina Wiltshire, Karen H. 2018-09-27 application/pdf https://doi.org/10.5194/hess-2016-254 https://www.hydrol-earth-syst-sci-discuss.net/hess-2016-254/ eng eng doi:10.5194/hess-2016-254 https://www.hydrol-earth-syst-sci-discuss.net/hess-2016-254/ eISSN: 1607-7938 Text 2018 ftcopernicus https://doi.org/10.5194/hess-2016-254 2019-12-24T09:52:19Z The water temperature characteristics of the Lena River at basin outlet during the summer season (June–September) are considered. The analysis is based on a long-term data series covering the period from the beginning of observation (1936) to the present time (2012) at Kusur (Kyusyur) gauging station and complementary data at several stations downstream and one station upstream. These additional data are rarely used, but their analysis is important for understanding processes in the basin outlet area. The differences between the stream surface temperatures at Kusur station and 200 km downstream to the north at Habarova (Khabarova) station have almost always been an anomalously large and negative for the considered period since the beginning of observation during open water season from July to September. The description of this difference and its analysis are presented. To sort the problem out, we consider the observational data in terms of the hydrology and morphology of the Lena River delta and main channel area and apply statistical and deterministic modelling approaches. The inability of water temperature observational data at Kusur station to represent the mean cross-sectional temperature is addressed. The analysis of the water temperature trends at the Kusur and Habarova stations is also presented. Text lena river Copernicus Publications: E-Journals Habarova ENVELOPE(21.917,21.917,-72.200,-72.200) Kyusyur ENVELOPE(127.364,127.364,70.688,70.688)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The water temperature characteristics of the Lena River at basin outlet during the summer season (June–September) are considered. The analysis is based on a long-term data series covering the period from the beginning of observation (1936) to the present time (2012) at Kusur (Kyusyur) gauging station and complementary data at several stations downstream and one station upstream. These additional data are rarely used, but their analysis is important for understanding processes in the basin outlet area. The differences between the stream surface temperatures at Kusur station and 200 km downstream to the north at Habarova (Khabarova) station have almost always been an anomalously large and negative for the considered period since the beginning of observation during open water season from July to September. The description of this difference and its analysis are presented. To sort the problem out, we consider the observational data in terms of the hydrology and morphology of the Lena River delta and main channel area and apply statistical and deterministic modelling approaches. The inability of water temperature observational data at Kusur station to represent the mean cross-sectional temperature is addressed. The analysis of the water temperature trends at the Kusur and Habarova stations is also presented.
format Text
author Fofonova, Vera
Zhilyaev, Igor
Krayneva, Marina
Yakshina, Dina
Tananaev, Nikita
Volkova, Nina
Wiltshire, Karen H.
spellingShingle Fofonova, Vera
Zhilyaev, Igor
Krayneva, Marina
Yakshina, Dina
Tananaev, Nikita
Volkova, Nina
Wiltshire, Karen H.
The water temperature characteristics of the Lena River at basin outlet in the summer period
author_facet Fofonova, Vera
Zhilyaev, Igor
Krayneva, Marina
Yakshina, Dina
Tananaev, Nikita
Volkova, Nina
Wiltshire, Karen H.
author_sort Fofonova, Vera
title The water temperature characteristics of the Lena River at basin outlet in the summer period
title_short The water temperature characteristics of the Lena River at basin outlet in the summer period
title_full The water temperature characteristics of the Lena River at basin outlet in the summer period
title_fullStr The water temperature characteristics of the Lena River at basin outlet in the summer period
title_full_unstemmed The water temperature characteristics of the Lena River at basin outlet in the summer period
title_sort water temperature characteristics of the lena river at basin outlet in the summer period
publishDate 2018
url https://doi.org/10.5194/hess-2016-254
https://www.hydrol-earth-syst-sci-discuss.net/hess-2016-254/
long_lat ENVELOPE(21.917,21.917,-72.200,-72.200)
ENVELOPE(127.364,127.364,70.688,70.688)
geographic Habarova
Kyusyur
geographic_facet Habarova
Kyusyur
genre lena river
genre_facet lena river
op_source eISSN: 1607-7938
op_relation doi:10.5194/hess-2016-254
https://www.hydrol-earth-syst-sci-discuss.net/hess-2016-254/
op_doi https://doi.org/10.5194/hess-2016-254
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