Hewer Micah J, Gough William A
Department of Physical and Environmental Sciences, University of Toronto at Scarborough, 1265 Military Trail, Toronto, ON M1C 1A4 Canada.
Theor Appl Climatol. 2023;151(1-2):47-64. doi: 10.1007/s00704-022-04267-2. Epub 2022 Nov 7.
Global temperatures are increasing, and regional precipitation patterns are changing. Snow is an excellent indicator of regional climate change; 50 years of temperature and precipitation data were analysed from weather stations located within the five most populated cities of Ontario (Canada). Recorded measurements for temperature and precipitation were converted into binary values to indicate the frequency of rain days, snow days, wet days (when total precipitation is greater than 0.2 mm) and freezing days (when the average temperature is less than 0 °C); then, these values were summed over each winter season from 1970/71 to 2019/20. The snow-day fraction was calculated from the seasonal totals by dividing the total number of snow days by the total number of wet days. Historical trends were detected using Pearson's , Kendall's Tau and Spearman's Rho. Differences in mean values between the first decade (1971-1980) and the last decade (2011-2020) within the time series for the snow-day fraction and total freezing days were determined using Student's -tests. During the winter season in southern Ontario (December 1 to March 31), total snow days, total wet days, the snow-day fraction and freezing days were all decreasing at statistically significant rates (90 to 99% confidence levels) across four of the five cities studied (Toronto, Ottawa, Hamilton and London). Mississauga was the exception, being the only city where rain days were increasing, but no trends were detected for snow days or wet days. The snow-day fraction was decreasing in Mississauga but not at a statistically significant rate, despite freezing days decreasing at the greatest rate compared to the other four cities. Total freezing days were highly correlated with the snow-day fraction during the winter season, being able to explain 61 to 76 percent of the observed variability, where Mississauga recorded the weakest correlation and London recorded the strongest correlation.
全球气温在上升,区域降水模式也在改变。降雪是区域气候变化的一个极佳指标;对位于加拿大安大略省人口最多的五个城市的气象站50年的气温和降水数据进行了分析。将记录的气温和降水测量值转换为二进制值,以表明雨日、雪日、湿日(总降水量大于0.2毫米时)和冰冻日(平均气温低于0°C时)的频率;然后,将这些值在1970/71至2019/20的每个冬季进行汇总。雪日比例是通过将雪日总数除以湿日总数,从季节性总数中计算得出的。使用皮尔逊相关系数、肯德尔秩相关系数和斯皮尔曼秩相关系数来检测历史趋势。使用学生t检验确定时间序列中雪日比例和总冰冻日的第一个十年(1971 - 1980年)和最后一个十年(2011 - 2020年)之间的平均值差异。在安大略省南部的冬季(12月1日至3月31日),在所研究的五个城市中的四个(多伦多、渥太华、汉密尔顿和伦敦),总雪日、总湿日、雪日比例和冰冻日都以具有统计学意义的速率下降(置信水平为90%至99%)。密西沙加是个例外,它是唯一一个雨日增加的城市,但未检测到雪日或湿日的趋势。密西沙加的雪日比例在下降,但未达到统计学显著速率,尽管与其他四个城市相比,其冰冻日下降速率最大。冬季总冰冻日与雪日比例高度相关,能够解释61%至76%的观测变异性,其中密西沙加的相关性最弱,伦敦的相关性最强。