Climate change in Nova Scotia: temperature increases from 1961 to 2020

D. Garbary, N. M. Hill
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引用次数: 2

Abstract

An analysis of temperature in Nova Scotia, using climate normals for 1961-1990 and temperature records from 1961 to 2020, is presented for 16 sites across the province. These records show a slight warming trend in the first 40 years from 6.0 ± 0.5 °C (1961-1990), followed by a more significant increase in average temperature post-1990 of 1.0 °C to 6.7 ± 0.5 °C, and to 7.0 ± 0.5 in the post-1998 period. A jump in average temperature in 1998 is such that in only a few following years did the mean annual temperature fall below the average annual temperature for the previous period. A step change was coincident with La Niña events and increasing Atlantic Ocean temperatures associated with a shift of the Atlantic Multi-decadal Oscillation into a positive phase. The increase in mean monthly temperatures was more apparent in the Autumn when first frosts were later and there were fewer days with frost. This led to a significant increase in continuous frost-free days of 9.2 ± 7.9 days, with increases ranging from 0.4 to 30.6 days. Relative to other sites, Yarmouth had the smallest annual increase in mean temperature, of 0.5 °C, but this was associated with a major increase in continuous frost-free days, of 11.3. Because overall temperature change was based largely on a step change post-1998, rather than a continuous, gradual change (seen only in frost-free days), it is difficult to calculate a rate, or to predict future patterns of temperature increases. We suggest a significant influence of El Niño Southern Oscillation and Atlantic Multi-decadal Oscillation as potential contributors to the temperature increase. Increases in annual temperature and seasonality are discussed in terms of flowering phenology, including flowering in the Spring of 2021 when 31 species were blooming by the end of April.Keywords: climate change, climate normal, flowering phenology, Nova Scotia, temperature, weather
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新斯科舍省的气候变化:1961年至2020年的气温上升
本文利用1961-1990年的气候正常值和1961- 2020年的温度记录,对新斯科舍省16个站点的温度进行了分析。这些记录显示,从6.0±0.5°C(1961-1990)开始,前40年有轻微的升温趋势,随后在1990年以后平均气温显著升高1.0°C至6.7±0.5°C, 1998年以后平均气温显著升高7.0±0.5°C。1998年的平均气温急剧上升,仅在随后的几年里,年平均气温才低于前一时期的年平均气温。阶跃变化与La Niña事件一致,大西洋温度升高与大西洋多年代际涛动向正相位的转变有关。月平均气温的上升在秋季更为明显,因为秋季初霜较晚,霜冻天数较少。这导致连续无霜天数显著增加,为9.2±7.9天,增加幅度为0.4 ~ 30.6天。相对于其他地点,雅茅斯的年平均温度增幅最小,为0.5°C,但这与连续无霜期的主要增加有关,为11.3天。由于总体温度变化主要基于1998年以后的阶跃变化,而不是连续的、渐进的变化(只在无霜期出现),因此很难计算出温度上升的速率,也很难预测未来温度上升的模式。我们认为El Niño南方涛动和大西洋多年代际涛动是温度升高的潜在贡献者。从开花物候学的角度讨论了年温度和季节性的增加,包括2021年春季的开花,当时31种植物在4月底开花。关键词:气候变化,气候常态,开花物候,新斯科舍省,温度,天气
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