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 long-term data series covering the period from the beginning of observation (1936) to the present time at Kusur (Kyusyur) station and complementa...
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ftawi:oai:epic.awi.de:42938 2024-09-15T18:17:42+00:00 The water temperature characteristics of the Lena River at basin outlet in the summer period Fofonova, Vera Zhilyaev, Igor Krainva, Marina Iakshina, Dina Tananaev, Nikita Volkova, Nina Wiltshire, Karen Helen 2016-12 application/pdf https://epic.awi.de/id/eprint/42938/ https://epic.awi.de/id/eprint/42938/1/Programvera.pdf https://hdl.handle.net/10013/epic.49487 https://hdl.handle.net/10013/epic.49487.d001 unknown https://epic.awi.de/id/eprint/42938/1/Programvera.pdf https://hdl.handle.net/10013/epic.49487.d001 Fofonova, V. orcid:0000-0002-5956-1844 , Zhilyaev, I. , Krainva, M. , Iakshina, D. , Tananaev, N. , Volkova, N. and Wiltshire, K. H. orcid:0000-0002-7148-0529 (2016) The water temperature characteristics of the Lena River at basin outlet in the summer period , ''East Siberian Shelf: observations, data analysis, modelling efforts, AWI, Bremerhaven, 7 December 2016 - 9 December 2016 . hdl:10013/epic.49487 EPIC3''East Siberian Shelf: observations, data analysis, modelling efforts, AWI, Bremerhaven, 2016-12-07-2016-12-09 Conference notRev 2016 ftawi 2024-06-24T04:16:35Z The water temperature characteristics of the Lena River at basin outlet during the summer season (June–September) are considered. The analysis is based on long-term data series covering the period from the beginning of observation (1936) to the present time at Kusur (Kyusyur) 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, apply statistical and deterministic modelling approaches. Conference Object lena river Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
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 long-term data series covering the period from the beginning of observation (1936) to the present time at Kusur (Kyusyur) 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, apply statistical and deterministic modelling approaches. |
format |
Conference Object |
author |
Fofonova, Vera Zhilyaev, Igor Krainva, Marina Iakshina, Dina Tananaev, Nikita Volkova, Nina Wiltshire, Karen Helen |
spellingShingle |
Fofonova, Vera Zhilyaev, Igor Krainva, Marina Iakshina, Dina Tananaev, Nikita Volkova, Nina Wiltshire, Karen Helen The water temperature characteristics of the Lena River at basin outlet in the summer period |
author_facet |
Fofonova, Vera Zhilyaev, Igor Krainva, Marina Iakshina, Dina Tananaev, Nikita Volkova, Nina Wiltshire, Karen Helen |
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 |
2016 |
url |
https://epic.awi.de/id/eprint/42938/ https://epic.awi.de/id/eprint/42938/1/Programvera.pdf https://hdl.handle.net/10013/epic.49487 https://hdl.handle.net/10013/epic.49487.d001 |
genre |
lena river |
genre_facet |
lena river |
op_source |
EPIC3''East Siberian Shelf: observations, data analysis, modelling efforts, AWI, Bremerhaven, 2016-12-07-2016-12-09 |
op_relation |
https://epic.awi.de/id/eprint/42938/1/Programvera.pdf https://hdl.handle.net/10013/epic.49487.d001 Fofonova, V. orcid:0000-0002-5956-1844 , Zhilyaev, I. , Krainva, M. , Iakshina, D. , Tananaev, N. , Volkova, N. and Wiltshire, K. H. orcid:0000-0002-7148-0529 (2016) The water temperature characteristics of the Lena River at basin outlet in the summer period , ''East Siberian Shelf: observations, data analysis, modelling efforts, AWI, Bremerhaven, 7 December 2016 - 9 December 2016 . hdl:10013/epic.49487 |
_version_ |
1810455784736161792 |