Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia
In the context of the Arctic amplification of climate change affecting the regional atmospheric hydrological cycle, it is crucial to characterize the present-day’s moisture sources of the Arctic. The isotopic composition is an important tool to enhance our understanding of the drivers of the hydrolo...
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ftcopernicus:oai:publications.copernicus.org:acpd80919 2023-05-15T15:00:47+02:00 Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia Bonne, Jean-Louis Meyer, Hanno Behrens, Melanie Boike, Julia Kipfstuhl, Sepp Rabe, Benjamin Schmidt, Toni Schönicke, Lutz Steen-Larsen, Hans Christian Werner, Martin 2020-01-06 application/pdf https://doi.org/10.5194/acp-2019-942 https://www.atmos-chem-phys-discuss.net/acp-2019-942/ eng eng doi:10.5194/acp-2019-942 https://www.atmos-chem-phys-discuss.net/acp-2019-942/ eISSN: 1680-7324 Text 2020 ftcopernicus https://doi.org/10.5194/acp-2019-942 2020-01-13T15:42:00Z In the context of the Arctic amplification of climate change affecting the regional atmospheric hydrological cycle, it is crucial to characterize the present-day’s moisture sources of the Arctic. The isotopic composition is an important tool to enhance our understanding of the drivers of the hydrological cycle, due to the different molecular characteristics of water stable isotopes during phase change. This study introduces two years of continuous in situ water vapour and precipitation isotopic observations conducted since July 2015 in the east-Siberian Lena delta, at the research station on the Samoylov Island. The vapour isotopic signals are dominated by variations at the seasonal and synoptic time scales. Diurnal variations of the vapour isotopic signals are masked by synoptic variations, indicating low variations of the amplitude of local sources at the diurnal scale in winter, summer and autumn. Low amplitude diurnal variations in spring may indicate exchange of moisture between the atmosphere and the snow-covered surface. Moisture sources diagnostics based on semi-Lagrangian backward trajectories reveal that different air mass origins have contrasted contributions to the moisture budget of the Lena delta region. At the seasonal scale, the distance from the net moisture sources to the arrival site strongly varies. During the coldest months, no contribution from local secondary evaporation is observed. Variations of the vapour isotopic composition during the cold season on synoptic time scale are strongly related to moisture source regions and variations in the atmospheric transport: warm and isotopically-enriched moist air is linked with fast transport from the Atlantic sector; while dry and cold air with isotopically-depleted moisture is generally associated to air masses moving slowly over northern Eurasia. Text Arctic Climate change lena delta lena river Siberia Copernicus Publications: E-Journals Arctic |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
In the context of the Arctic amplification of climate change affecting the regional atmospheric hydrological cycle, it is crucial to characterize the present-day’s moisture sources of the Arctic. The isotopic composition is an important tool to enhance our understanding of the drivers of the hydrological cycle, due to the different molecular characteristics of water stable isotopes during phase change. This study introduces two years of continuous in situ water vapour and precipitation isotopic observations conducted since July 2015 in the east-Siberian Lena delta, at the research station on the Samoylov Island. The vapour isotopic signals are dominated by variations at the seasonal and synoptic time scales. Diurnal variations of the vapour isotopic signals are masked by synoptic variations, indicating low variations of the amplitude of local sources at the diurnal scale in winter, summer and autumn. Low amplitude diurnal variations in spring may indicate exchange of moisture between the atmosphere and the snow-covered surface. Moisture sources diagnostics based on semi-Lagrangian backward trajectories reveal that different air mass origins have contrasted contributions to the moisture budget of the Lena delta region. At the seasonal scale, the distance from the net moisture sources to the arrival site strongly varies. During the coldest months, no contribution from local secondary evaporation is observed. Variations of the vapour isotopic composition during the cold season on synoptic time scale are strongly related to moisture source regions and variations in the atmospheric transport: warm and isotopically-enriched moist air is linked with fast transport from the Atlantic sector; while dry and cold air with isotopically-depleted moisture is generally associated to air masses moving slowly over northern Eurasia. |
format |
Text |
author |
Bonne, Jean-Louis Meyer, Hanno Behrens, Melanie Boike, Julia Kipfstuhl, Sepp Rabe, Benjamin Schmidt, Toni Schönicke, Lutz Steen-Larsen, Hans Christian Werner, Martin |
spellingShingle |
Bonne, Jean-Louis Meyer, Hanno Behrens, Melanie Boike, Julia Kipfstuhl, Sepp Rabe, Benjamin Schmidt, Toni Schönicke, Lutz Steen-Larsen, Hans Christian Werner, Martin Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia |
author_facet |
Bonne, Jean-Louis Meyer, Hanno Behrens, Melanie Boike, Julia Kipfstuhl, Sepp Rabe, Benjamin Schmidt, Toni Schönicke, Lutz Steen-Larsen, Hans Christian Werner, Martin |
author_sort |
Bonne, Jean-Louis |
title |
Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia |
title_short |
Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia |
title_full |
Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia |
title_fullStr |
Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia |
title_full_unstemmed |
Moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the Lena River Delta, Siberia |
title_sort |
moisture origin as a driver of temporal variabilities of the water vapour isotopic composition in the lena river delta, siberia |
publishDate |
2020 |
url |
https://doi.org/10.5194/acp-2019-942 https://www.atmos-chem-phys-discuss.net/acp-2019-942/ |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change lena delta lena river Siberia |
genre_facet |
Arctic Climate change lena delta lena river Siberia |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-2019-942 https://www.atmos-chem-phys-discuss.net/acp-2019-942/ |
op_doi |
https://doi.org/10.5194/acp-2019-942 |
_version_ |
1766332848647700480 |