Wang Hua, Chen Hui Hua, Tang Li Sheng, Wang Juan Huai, Tang Hai Yan
Guangdong Climate Center, Guangzhou 510080, China.
Ying Yong Sheng Tai Xue Bao. 2018 Jan;29(1):93-102. doi: 10.13287/j.1001-9332.201801.015.
Trend analysis method was applied to analyze the general variation characteristics of the climate resources and meteorological disasters of growing season of the winter planting in Guangdong before (1961-1996) and after climate warming (1997-2015). Percentile method was employed to determine thresholds for extreme cold and drought in major planting regions, and the characteristics of extreme disasters since climate warming were analyzed. The results showed that, by comparing 1997-2015 with 1961-1996, the heat value in winter growing season increased significantly. The belt with a higher heat value, where the average temperature was ≥15 ℃ and accumulated temperature was ≥2200 ℃·d, covered the main winter production regions as Shaoguan, Zhanjiang, Maoming, Huizhou, Meizhou and Guangzhou. Meanwhile, the precipitation witnessed a slight increase. The regions with precipitations of 250-350 mm included Zhanjiang, Maoming, Huizhou, Guangzhou and Meizhou. Chilling injury in the winter planting season in the regions decreased, the belt with an accumulated chilling of <2 ℃·d covered the major geographic parts of the involved regions as Zhanjiang, Maoming, Guangzhou and Huizhou; and the belt with an accumulated chilling of 8-16 ℃·d covered the major geographic parts of Shaoguan and Meizhou. Meanwhile, the drought days decreased, the belt with drought days ≥50 included the major geographic parts of Zhanjiang, Maoming, Huizhou, Guangzhou and the belt with drought days <50 included the major geographic parts of Shaoguan. The typical case of the extreme disasters showed that the extreme chilling injury and drought in the main producing regions should not be overlooked. Maoming, Huizhou and Meizhou were at higher risk of extreme chilling injury, followed by Shaoguan and Guangzhou. Zhanjiang and Maoming faced the highest risk of extreme drought, Huizhou and Guangzhou took the second place, Shaoguan and Meizhou went last. During 1997-2015, the heat of winter season increased significantly, the trend of chilling and drought decreased, however, the extreme disasters occurred frequently and the risks were higher in winter production areas. It was suggested that the winter planting should be closely integrated with climate resources and the occurrence law of meteorological disasters in growing season.
运用趋势分析方法,分析广东冬季种植生长季在气候变暖前(1961—1996年)和气候变暖后(1997—2015年)气候资源与气象灾害的总体变化特征。采用百分位法确定主要种植区极端低温和干旱阈值,分析气候变暖以来极端灾害特征。结果表明,与1961—1996年相比,1997—2015年冬季生长季热量值显著增加,平均气温≥15℃、积温≥2200℃·d的高热量值带覆盖韶关、湛江、茂名、惠州、梅州和广州等主要冬季产区。同时,降水量略有增加,降水量250~350mm的区域包括湛江、茂名、惠州、广州和梅州。冬季种植季各区域冷害减少,累计冷害<2℃·d的地带覆盖湛江、茂名、广州和惠州等涉及区域的主要地理部分;累计冷害8~16℃·d的地带覆盖韶关和梅州的主要地理部分。同时,干旱日数减少,干旱日数≥50d的地带包括湛江、茂名、惠州、广州的主要地理部分,干旱日数<50d的地带包括韶关的主要地理部分。极端灾害典型案例表明,主产区极端冷害和干旱不容小觑。茂名、惠州和梅州极端冷害风险较高,其次是韶关和广州。湛江和茂名极端干旱风险最高,惠州和广州次之,韶关和梅州最低。1997—2015年,冬季热量显著增加,冷害和干旱呈减少趋势,但极端灾害频发,冬季产区风险较高。建议冬季种植应与气候资源及生长季气象灾害发生规律紧密结合。