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Effects of recent warm and cold spells on European plant phenology

机译:最近的冷热天气对欧洲植物物候的影响

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Climate change is already altering the magnitude and/or frequency of extreme events which will in turn affect plant fitness more than any change in the average. Although the fingerprint of anthropogenic warming in recent phenological records is well understood, the impacts of extreme events have been largely neglected. Thus, the temperature response of European phenological records to warm and cold spells was studied using the COST725 database. We restricted our analysis to the period 1951-2004 due to better spatial coverage. Warm and cold spells were identified using monthly mean ENSEMBLES temperature data on a 0.5 degrees grid for Europe. Their phenological impact was assessed as anomalies from maps displaying mean onsets for 1930-1939. Our results clearly exhibit continental cold spells predominating in the period 1951-1988, especially during the growing season, whereas the period from 1989 onwards was mainly characterised by warm spells in all seasons. The impacts of these warm/cold spells on the onset of phenological seasons differed strongly depending on species, phase and timing. "False" phases such as the sowing of winter cereals hardly reacted to summer warm/cold spells; only the sowing of summer cereals mirrored spring temperature warm/cold spells. The heading dates of winter cereals did not reveal any consistent results probably due to fewer warm/cold spells identified in the relevant late spring months. Apple flowering and the harvest of winter cereals were the best indicators of warm/cold spells in early spring and summer, also being spatially coherent with the patterns of warm/cold spells.CT International Conference on Phenology - Climate Change Impacts and AdaptationCY JUN, 2010CL Trinity Coll, Dublin, IRELANDHO Trinity Coll
机译:气候变化已经在改变极端事件的严重程度和/或频率,这反过来比平均水平的任何变化对植物适应性的影响更大。尽管在最近的物候记录中人为变暖的指纹已广为人知,但极端事件的影响已被很大程度上忽略。因此,使用COST725数据库研究了欧洲物候记录对冷热天气的温度响应。由于更好的空间覆盖范围,我们将分析限制在1951-2004年。使用欧洲0.5度网格上的ENSEMBLES每月平均温度数据来识别冷热天气。他们的物候影响被评估为显示1930-1939年平均发病时间的地图异常。我们的结果清楚地表明,在1951年至1988年期间,尤其是在生长季节期间,大陆的寒冷季节占主导地位,而从1989年开始的时期主要表现为所有季节的温暖季节。这些暖/冷法术对物候季节发作的影响因物种,阶段和时间而异。冬季谷物的播种等“假”阶段对夏季的温暖/寒冷季节几乎没有反应。只有夏季谷物的播种反映了春季温度的温暖/寒冷。冬季谷物的抽穗日期未显示出任何一致的结果,这可能是由于在相关的春季末期识别出的温暖/寒冷季节减少了。苹果花期和冬季谷物的收成是春季和夏季初温/冷季节的最好指标,并且在空间上与温/冷季节的模式保持一致。CT国际物候学会议-气候变化影响与适应CY Jun,2010CL Trinity Coll,都柏林,爱尔兰

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