Analysis of Precipitation Forms Characteristics in Heilongjiang Province based on Snowfall/Precipitation Ratio

  • HOU Bingfei ,
  • JIANG Chao ,
  • SUN Jianxin
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  • Forestry college, Beijing forestry university, Beijing 100083, China

Received date: 2018-01-26

  Online published: 2019-08-28

Abstract

The precipitation form (snowfall, rainfall or fleet) have greatly influenced a large number of ecological processes, such as surface runoff, energy flow, and material circulation processes. Obviously, precipitation form is very sensitive to temperature changes. To discuss the effects of climate change on precipitation form, a dataset including average daily rainfall and temperature data of 27 stations from 1960 to 2015 in Heilongjiang province was employed to analyze the long-term change in annual snowfall and snowfall/rainfall ratio. The results indicate that:The annual mean snowfall in Heilongjiang province experienced a sharp growth with 34.3% increase after a break which occurred around the year 2003. The long-term increase rate was 3.3 mm per decade. On the contrary, no significant change was observed in annual mean rainfall in Heilongjiang province. Trend tests showed a 7.6% per decade significant increase in snowfall/rainfall ratio in Heilongjiang. The main characteristic of change in snowfall spatial distribution was consistent upward trend except Huma station, but the amplitude of eastern parts was larger than the western ones. Otherwise, rainfall variation spatial pattern was differed among regions. In general the changes in the southern part were more strongly than the northern. The variation of fleet presented a distinct trend of decreasing from east to west. There was a large difference in fleet between the two sides of The Changbai-Hinggan mountains, presented as a sharp decline from the eastern part of the mountain to the western. The difference in spatial distribution between snowfall/rainfall ratio and snowfall was mainly reflected in the areas where rainfall was significant decreased, such as the western foot of Changbai mountains, where the rain shadow effect was extremely strong. The common impacts of delayed origin date and advanced end date resulted in the snowfall season range evidently shortened about 18 days in the last 56 years. The reason may be attributed to a significant temperature rise in Heilongjiang province. The spring warming should be considered as a major role rather than autumn because of the higher temperature variation, especially the increase in minimum temperature. There was no significantly change observed in average annual snowfall days. The amplitude changed in snowfall frequency in the northern was larger than the southern. Consistent with the snowfall growth, an increased trend of snowfall intensity was found in Heilongjiang, with a changing rate of 0.8 mm per decade. In the context of global warming, higher snowfall rate phenomenon was observed in Heilongjiang province.

Cite this article

HOU Bingfei , JIANG Chao , SUN Jianxin . Analysis of Precipitation Forms Characteristics in Heilongjiang Province based on Snowfall/Precipitation Ratio[J]. Plateau Meteorology, 2019 , 38(4) : 781 -793 . DOI: 10.7522/j.issn.1000-0534.2018.00103

References

[1]Arnell N W, Brown S, Gosling S N, et al, 2016. The impacts of climate change across the globe:A multi-sectoral assessment[J]. Climatic Change, 134(3):457-474.
[2]Berghuijs W R, Woods R A, Hrachowitz M, 2014. A precipitation shift from snow towards rain leads to a decrease in streamflow[J]. Nature Climate Change, 4(7):583-586.
[3]Dai A G, 2008. Temperature and pressure dependence of the rain-snow phase transition over land and ocean[J]. Geophysical Research Letters, 35(12):62-77.
[4]Ding B H, Yang K, Qin J, et al, 2014. The dependence of precipitation types on surface elevation and meteorological conditions and its parameterization[J]. Journal of Hydrology, 513:154-163.
[5]Dingman S L, 2015. Physical Hydrology[M]. Long Grove:Waveland Press.
[6]Easterling D R, 2002. Recent changes in frost days and the frostfree season in the United States[J]. Bulletin of the American Meteorological Society, 83(9):1327-1332.
[7]Feng S, Hu Q, 2007. Changes in winter snowfall/precipitation ratio in the contiguous United States[J]. Journal of Geophysical Research Atmospheres, 112:D15109.
[8]Guo L, Li L, 2015. Variation of the proportion of precipitation occurring as snow in the Tian Shan Mountains, China[J]. International Journal of Climatology, 35(7):1379-1393.
[9]Gustafsson D, St?hli M, Jansson P E, 2001. The surface energy balance of a snow cover:Comparing measurements to two different simulation models[J]. Theoretical and Applied Climatology, 70(1/4):81-96.
[10]Huntington T G, Hodgkins G A, Keim B D, et al, 2004. Changes in the proportion of precipitation occurring as snow in New England (1949-2000)[J]. Journal of Climate, 17(17):2626-2636.
[11]Karl T R, Groisman P Y, Knight R W, et al, 1993. Recent variations of snow cover and snowfall in North America and their relation to precipitation and temperature variations[J]. Journal of Climate, 6(6):1327-1344.
[12]Ke C Q, Yu T, Yu K, et al, 2009. Snowfall trends and variability in Qinghai, China[J]. Theoretical and Applied Climatology, 98(3/4):251-258.
[13]Mizukami N, Koren V, Smith M, et al, 2013. The impact of precipitation type discrimination on hydrologic simulation:Rain-snow partitioning derived from HMT-west radar-detected bright band height versus surface temperature data[J]. Journal of Hydrometeorology, 14(4):1139-1158.
[14]Rauber R M, Olthoff L S, Ramamurthy M K, et al, 2001. Further investigation of a physically based, non-dimensional parameter for discriminating between locations of freezing rain and ice pellets[J]. Weather and Forecasting, 16(1):185-191.
[15]Scherrer S C, Appenzeller C, 2006. Swiss Alpine snow pack variability:Major patterns and links to local climate and large-scale flow[J]. Climate Research, 32(3):187-199. DOI:10.3354/cr032187.
[16]Screen J A, Simmonds I, 2012. Declining summer snowfall in the Arctic:Causes, impacts and feedbacks[J]. Climate Dynamics, 38(11/12):2243-2256.
[17]Serquet G, Marty C, Dulex J P, et al, 2011. Seasonal trends and temperature dependence of the snowfall/precipitation-day ratio in Switzerland[J]. Geophysical Research Letters, 38(7):128-136. DOI:10.1029/2011GL046976.
[18]Takeuchi Y, 2008. High correlation between winter precipitation and air temperature in heavy-snowfall areas in Japan[J]. Annals of Glaciology, 49(1):7-10.
[19]Wang J, Zhang M J, Wang S J, et al, 2016. Decrease in snowfall/rainfall ratio in the Tibetan Plateau from 1961 to 2013[J]. Acta Geographica Sinica, 26(9):1277-1288.
[20]Xu C, Chen Y, Li W, et al, 2008. Potential impact of climate change on snow cover area in the Tarim River basin[J]. Environmental Geology, 53(7):1465-1474.
[21]Yamazaki T, 2001. A one-dimensional land surface model adaptable to intensely cold regions and its applications in Eastern Siberia[J]. Journal of the Meteorological Society of Japan, 79:1107-1118.
[22]Yang Z L, Dickinson R E, Robock A, et al, 1997. Validation of the snow submodel of the biosphere-atmosphere transfer scheme with Russian snow cover and meteorological observational data[J]. Journal of Climate, 10(2):353-373.
[23]曹蓉, 2014.东北夏季降水的基本特征及其与大气环流和太平洋海温的关系[D].南京: 南京信息工程大学.
[24]胡婷, 2008.中国区域气溶胶的光学厚度特征和气候效应研究[D].南京: 南京信息工程大学.
[25]姜江, 姜大膀, 林一骅, 2015. 1961-2009年中国季风区范围和季风降水变化[J].大气科学, 39(4):722-730.
[26]李丹华, 文莉娟, 隆霄, 等, 2017.积雪对玛曲局地微气象特征影响的观测研究[J].高原气象, 36(2):330-339. DOI:10.7522/j.issn.1000-0534.2016.00074
[27]罗云峰, 吕达仁, 周秀骥, 等, 2002. 30年来我国大气气溶胶光学厚度平均分布特征分析[J].大气科学, 26(6):721-730.
[28]那济海, 周秀杰, 吴玉影, 2013.黑龙江省夏季6, 7, 8月降水与全国雨型变化关系分析[J].自然灾害学报, 22 (6):151-160.
[29]沈柏竹, 林中达, 陆日宇, 等, 2011.影响东北初夏和盛夏降水年际变化的环流特征分析[J].中国科学:地球科学, 41(3):402-412. DOI:10.1007/s11430-011-4173-6.
[30]孙秀忠, 罗勇, 张霞, 等, 2010. 1960-2005年东北地区降雪变化特征研究[J].气象与环境学报, 26(1):1-5.
[31]孙照渤, 曹蓉, 倪东鸿, 2016.东北夏季降水分型及其大气环流特征[J].大气科学学报, 39(1):18-27.
[32]王会军, 贺圣平, 2012. ENSO和东亚冬季风之关系在20世纪70年代中期之后的减弱[J].科学通报, 57(19):1713-1718.
[33]王继志, 李多, 杨元琴, 等, 2011.中国北方地区冬季雨雪年度变化与大气气溶胶分布特征研究[J].气象与环境学报, 27(6):66-71.
[34]王杰, 张明军, 王圣杰, 等, 2017. 1961-2013年新疆雪雨比变化[J].干旱区研究, 34(4):889-897.
[35]于成龙, 刘丹, 马秋斯, 等, 2016. 1961-2013年黑龙江省气温变化特征[J].环境科学与技术, 39(5):169-175.
[36]张宸赫, 赵天良, 王富, 等, 2017. 2003-2014年东北三省气溶胶光学厚度变化分析[J].环境科学, 38(2):476-484.
[37]张俊兰, 彭军, 2017.北疆春季降水相态转换判识和成因分析[J].高原气象, 36(4):939-949. DOI:10.7522/j.issn.1000-0534.2016.00094.
[38]张淑杰, 张玉书, 陈鹏狮, 等, 2011.东北地区湿润指数及其干湿界线的变化特征[J].干旱地区农业研究, 29(3):226-232.
[39]张雪婷, 李雪梅, 高培, 等, 2017.基于不同方法的中国天山山区降水形态分离研究[J].冰川冻土, 39(2):235-244.
[40]郑丽娜, 杨成芳, 刘畅, 2016.山东冬半年回流降雪形势特征及相关降水相态[J].高原气象, 35(2):520-527. DOI:10.7522/j.issn.1000-0534.2015.00055.
[41]郑小波, 周成霞, 罗宇翔, 等, 2011.中国各省区近10年遥感气溶胶光学厚度和变化[J].生态环境学报, 20(4):595-599.
[42]邹旭东, 张飞民, 王澄海, 等, 2013.我国东北地区冬季降水和东亚冬季风的关系研究[J].冰川冻土, 35(6):1454-1461.
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