Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-Arctic
Observational data from the Russian sub-Arctic stations are used to investigate long-term variability of the growing season length (GSL) and the number of frost days (FD) in 1949-2013. Consistent with the global warming pattern we find a trend-like increase (decrease) of GSL (FD) which is evident si...
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Format: | Article |
Language: | English |
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Lomonosov Moscow State University
2019-03-01
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Series: | Geography, Environment, Sustainability |
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Online Access: | https://ges.rgo.ru/jour/article/view/660 |
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author | I. I. Zveryaev A. V. Arkhipkin |
author_facet | I. I. Zveryaev A. V. Arkhipkin |
author_sort | I. I. Zveryaev |
collection | DOAJ |
description | Observational data from the Russian sub-Arctic stations are used to investigate long-term variability of the growing season length (GSL) and the number of frost days (FD) in 1949-2013. Consistent with the global warming pattern we find a trend-like increase (decrease) of GSL (FD) which is evident since early 1970th of the last century. These trendlike changes are best pronounced at Western stations (i.e. in European Russia and western Siberia) and they are essentially smaller to the East. Although we find some significant links to regional teleconnections (such as Scandinavian, East Atlantic and West Pacific teleconnections), in general our results imply rather weak impact of large scale atmospheric dynamics on interannual variability of GSL and FD. Further analysis of correlations between GSL and FD on the one side and snow cover on the other side revealed generally stronger links to snow cover compared to teleconnections. However, revealed links to regional atmospheric teleconnections and snow cover are significantly impacted by the linear trends. In general, our results imply that compared to large scale atmospheric dynamics impacting interannual variability, snow cover (being a result of wintertime synoptic activity) plays a more important role in decadal-interdecadal variations of GSL and FD in Russian sub-Arctic, which may have some value regarding predictability of the summer climate in the region. |
first_indexed | 2024-04-10T02:33:24Z |
format | Article |
id | doaj.art-398f0639b73d481bb4f31e7b1a107b85 |
institution | Directory Open Access Journal |
issn | 2071-9388 2542-1565 |
language | English |
last_indexed | 2024-04-10T02:33:24Z |
publishDate | 2019-03-01 |
publisher | Lomonosov Moscow State University |
record_format | Article |
series | Geography, Environment, Sustainability |
spelling | doaj.art-398f0639b73d481bb4f31e7b1a107b852023-03-13T07:52:32ZengLomonosov Moscow State UniversityGeography, Environment, Sustainability2071-93882542-15652019-03-01121132210.24057/2071-9388-2018-55349Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-ArcticI. I. Zveryaev0A. V. Arkhipkin1Shirshov Institute of Oceanology, Russian Academy of SciencesShirshov Institute of Oceanology, Russian Academy of SciencesObservational data from the Russian sub-Arctic stations are used to investigate long-term variability of the growing season length (GSL) and the number of frost days (FD) in 1949-2013. Consistent with the global warming pattern we find a trend-like increase (decrease) of GSL (FD) which is evident since early 1970th of the last century. These trendlike changes are best pronounced at Western stations (i.e. in European Russia and western Siberia) and they are essentially smaller to the East. Although we find some significant links to regional teleconnections (such as Scandinavian, East Atlantic and West Pacific teleconnections), in general our results imply rather weak impact of large scale atmospheric dynamics on interannual variability of GSL and FD. Further analysis of correlations between GSL and FD on the one side and snow cover on the other side revealed generally stronger links to snow cover compared to teleconnections. However, revealed links to regional atmospheric teleconnections and snow cover are significantly impacted by the linear trends. In general, our results imply that compared to large scale atmospheric dynamics impacting interannual variability, snow cover (being a result of wintertime synoptic activity) plays a more important role in decadal-interdecadal variations of GSL and FD in Russian sub-Arctic, which may have some value regarding predictability of the summer climate in the region.https://ges.rgo.ru/jour/article/view/660growing seasonfrost dayssnow coverteleconnectionsnorthern eurasiaclimate variability and change |
spellingShingle | I. I. Zveryaev A. V. Arkhipkin Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-Arctic Geography, Environment, Sustainability growing season frost days snow cover teleconnections northern eurasia climate variability and change |
title | Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-Arctic |
title_full | Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-Arctic |
title_fullStr | Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-Arctic |
title_full_unstemmed | Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-Arctic |
title_short | Variability and Changes of the Growing Season Length and Frost Days Number in Russian sub-Arctic |
title_sort | variability and changes of the growing season length and frost days number in russian sub arctic |
topic | growing season frost days snow cover teleconnections northern eurasia climate variability and change |
url | https://ges.rgo.ru/jour/article/view/660 |
work_keys_str_mv | AT iizveryaev variabilityandchangesofthegrowingseasonlengthandfrostdaysnumberinrussiansubarctic AT avarkhipkin variabilityandchangesofthegrowingseasonlengthandfrostdaysnumberinrussiansubarctic |