Variability in snow cover phenology in China from 1952 to 2010

Daily snow observation data from 672 stations in China, particularly the 296 stations with over 10 mean snow cover days (SCDs) in a year during the period of 1952–2010, are used in this study. We first examine spatiotemporal variations and trends of SCDs, snow cover onset date (SCOD), and snow cover...

Full description

Bibliographic Details
Published in:Hydrology and Earth System Sciences
Main Authors: C.-Q. Ke, X.-C. Li, H. Xie, D.-H. Ma, X. Liu, C. Kou
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
T
G
Online Access:https://doi.org/10.5194/hess-20-755-2016
https://doaj.org/article/79272c4edd2c491ca800d0ccc25dfc00
id ftdoajarticles:oai:doaj.org/article:79272c4edd2c491ca800d0ccc25dfc00
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:79272c4edd2c491ca800d0ccc25dfc00 2023-05-15T15:11:21+02:00 Variability in snow cover phenology in China from 1952 to 2010 C.-Q. Ke X.-C. Li H. Xie D.-H. Ma X. Liu C. Kou 2016-02-01T00:00:00Z https://doi.org/10.5194/hess-20-755-2016 https://doaj.org/article/79272c4edd2c491ca800d0ccc25dfc00 EN eng Copernicus Publications http://www.hydrol-earth-syst-sci.net/20/755/2016/hess-20-755-2016.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 1027-5606 1607-7938 doi:10.5194/hess-20-755-2016 https://doaj.org/article/79272c4edd2c491ca800d0ccc25dfc00 Hydrology and Earth System Sciences, Vol 20, Iss 2, Pp 755-770 (2016) Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2016 ftdoajarticles https://doi.org/10.5194/hess-20-755-2016 2022-12-31T12:43:50Z Daily snow observation data from 672 stations in China, particularly the 296 stations with over 10 mean snow cover days (SCDs) in a year during the period of 1952–2010, are used in this study. We first examine spatiotemporal variations and trends of SCDs, snow cover onset date (SCOD), and snow cover end date (SCED). We then investigate the relationships of SCDs with number of days with temperature below 0 °C (TBZD), mean air temperature (MAT), and Arctic Oscillation (AO) index. The results indicate that years with a positive anomaly of SCDs for the entire country include 1955, 1957, 1964, and 2010, and years with a negative anomaly of SCDs include 1953, 1965, 1999, 2002, and 2009. The reduced TBZD and increased MAT are the main reasons for the overall late SCOD and early SCED since 1952. This explains why only 12 % of the stations show significant shortening of SCDs, while 75 % of the stations show no significant change in the SCDs trends. Our analyses indicate that the distribution pattern and trends of SCDs in China are very complex and are not controlled by any single climate variable examined (i.e. TBZD, MAT, or AO), but a combination of multiple variables. It is found that the AO has the maximum impact on the shortening trends of SCDs in the Shandong peninsula, Changbai Mountains, Xiaoxingganling, and north Xinjiang, while the combined TBZD and MAT have the maximum impact on the shortening trends of SCDs in the Loess Plateau, Tibetan Plateau, and Northeast Plain. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Hydrology and Earth System Sciences 20 2 755 770
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
spellingShingle Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
C.-Q. Ke
X.-C. Li
H. Xie
D.-H. Ma
X. Liu
C. Kou
Variability in snow cover phenology in China from 1952 to 2010
topic_facet Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
description Daily snow observation data from 672 stations in China, particularly the 296 stations with over 10 mean snow cover days (SCDs) in a year during the period of 1952–2010, are used in this study. We first examine spatiotemporal variations and trends of SCDs, snow cover onset date (SCOD), and snow cover end date (SCED). We then investigate the relationships of SCDs with number of days with temperature below 0 °C (TBZD), mean air temperature (MAT), and Arctic Oscillation (AO) index. The results indicate that years with a positive anomaly of SCDs for the entire country include 1955, 1957, 1964, and 2010, and years with a negative anomaly of SCDs include 1953, 1965, 1999, 2002, and 2009. The reduced TBZD and increased MAT are the main reasons for the overall late SCOD and early SCED since 1952. This explains why only 12 % of the stations show significant shortening of SCDs, while 75 % of the stations show no significant change in the SCDs trends. Our analyses indicate that the distribution pattern and trends of SCDs in China are very complex and are not controlled by any single climate variable examined (i.e. TBZD, MAT, or AO), but a combination of multiple variables. It is found that the AO has the maximum impact on the shortening trends of SCDs in the Shandong peninsula, Changbai Mountains, Xiaoxingganling, and north Xinjiang, while the combined TBZD and MAT have the maximum impact on the shortening trends of SCDs in the Loess Plateau, Tibetan Plateau, and Northeast Plain.
format Article in Journal/Newspaper
author C.-Q. Ke
X.-C. Li
H. Xie
D.-H. Ma
X. Liu
C. Kou
author_facet C.-Q. Ke
X.-C. Li
H. Xie
D.-H. Ma
X. Liu
C. Kou
author_sort C.-Q. Ke
title Variability in snow cover phenology in China from 1952 to 2010
title_short Variability in snow cover phenology in China from 1952 to 2010
title_full Variability in snow cover phenology in China from 1952 to 2010
title_fullStr Variability in snow cover phenology in China from 1952 to 2010
title_full_unstemmed Variability in snow cover phenology in China from 1952 to 2010
title_sort variability in snow cover phenology in china from 1952 to 2010
publisher Copernicus Publications
publishDate 2016
url https://doi.org/10.5194/hess-20-755-2016
https://doaj.org/article/79272c4edd2c491ca800d0ccc25dfc00
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Hydrology and Earth System Sciences, Vol 20, Iss 2, Pp 755-770 (2016)
op_relation http://www.hydrol-earth-syst-sci.net/20/755/2016/hess-20-755-2016.pdf
https://doaj.org/toc/1027-5606
https://doaj.org/toc/1607-7938
1027-5606
1607-7938
doi:10.5194/hess-20-755-2016
https://doaj.org/article/79272c4edd2c491ca800d0ccc25dfc00
op_doi https://doi.org/10.5194/hess-20-755-2016
container_title Hydrology and Earth System Sciences
container_volume 20
container_issue 2
container_start_page 755
op_container_end_page 770
_version_ 1766342219620417536