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首页> 外文期刊>Fresenius environmental bulletin >STUDY ON THE TREND OF VEGETATION PHENOLOGICAL CHANGE AND ITS RESPONSE TO CLIMATE CHANGE IN CHANGBAI MOUNTAINS
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STUDY ON THE TREND OF VEGETATION PHENOLOGICAL CHANGE AND ITS RESPONSE TO CLIMATE CHANGE IN CHANGBAI MOUNTAINS

机译:长白山植被物候变化趋势及其对气候变化的响应研究

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摘要

As one of the sensitive indicators in response to climate change, plant phonological change is usually used as an important component of dynamic vegetation models to reflect the dynamic of carbon and water exchange between the land surface and the atmosphere. The phenological change in large scale can not only reflect the seasonal variation patterns of vegetation, but also be an indicator of global climate change. In this study, using the biweekly NOAA/GIMMS NDVI (Normalized Difference Vegetation Index) and meteorological data, we employed the maximum rate of change to extract the phenological change of the vegetation types in Changbai Mountains during 1982-2006, and investigated the possible impact of recent climate change on growing season in three climate zones based on Jingyun Zheng’s climatic regionalization. The results were as follows: the onset date of green-up for the vegetation in warm temperate zone was in late April and the onset date of dormancy ended in late October. The length of growing season (LOS) for the vegetation types became shorter with increasing latitude. The earlier onset dates of green-up for all vegetation types were found in three climate zones during 1982-2006, ranging from 0.642 day/yr in Zone I, 0.429 day/yr in Zone II, to 0.371 day/yr in Zone II, which indicates that the earlier onset dates of green-up were significant with a longitude trend of vegetation types. The LOS of the three climate zones became longer during 1982-2006, but the lengthening of growing season demonstrated in different ways in the three climate zones. Temperature had stronger effect on the phenological change. The onset date of green-up was earlier and the corresponding temperature threshold was higher in the low latitude, and the LOS was in significant correlation with the accumulated temperature above 10? in three climate zones.
机译:植物物候变化作为响应气候变化的敏感指标之一,通常被用作动态植被模型的重要组成部分,以反映地表与大气之间的碳和水交换动态。物候的大范围变化不仅可以反映植被的季节变化规律,而且可以作为全球气候变化的指标。在这项研究中,我们使用每两周一次的NOAA / GIMMS NDVI(归一化植被指数)和气象数据,以最大变化率来提取1982-2006年长白山植被类型的物候变化,并研究了可能的影响郑经云的气候区划对三个气候带近期气候变化的影响结果如下:温带温带植被绿化的起始日期为四月下旬,休眠的起始日期为十月下旬。随着纬度的增加,植被类型的生长期(LOS)变短。在1982-2006年期间,在三个气候区中发现了所有植被类型的较早绿化开始日期,范围从I区的0.642天/年,II区的0.429天/年到II区的0.371天/年,这表明绿化的较早发生日期具有明显的植被类型的经度趋势。在1982-2006年期间,三个气候区的LOS变长了,但是三个气候区以不同的方式证明了生长期的延长。温度对物候变化的影响更大。在低纬度地区,绿化的发生日期较早,相应的温度阈值较高,LOS与累积温度高于10?C显着相关。在三个气候区。

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