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气候变化对日本北部白纹伊蚊(双翅目:蚊科)分布的影响:回顾性分析。

Impact of climate change on the distribution of Aedes albopictus (Diptera: Culicidae) in northern Japan: retrospective analyses.

出版信息

J Med Entomol. 2014 May;51(3):572-9. doi: 10.1603/me13178.

Abstract

The impact of climate change on the distribution of Aedes albopictus (Skuse) was analyzed in northern Japan, where chronological distribution records are incomplete. We analyzed local climate data using linear regression of the thermal suitability index (TSI) for the mosquito and mean annual temperature as functions of time. In northern Japan, thermal conditions since the early 20th century have become increasingly suitable for Ae. albopictus, more as a result of decreasing coldness in the overwintering season than increasing warmth in the reproductive season. Based on recent discovery records of Ae. albopictus in the northern border range, we determined thermal criteria for estimating when its persistent establishment became thermally possible. Retrospective analyses indicated that those criteria were reached in most coastal lowlands of northern Honshu before the accelerated temperature increase after the mid-1980s and the first records of this species after 1990; at some sites, temperature criteria were reached during or before the early 20th century. Expansion of the thermally suitable range after 1990 was supported only for inland areas and the northernmost Pacific coast. The estimated expansion rate was approximately 26 km per decade. Our analyses also demonstrated the importance of local climate heterogeneity (apart from north-south or altitudinal temperature gradients) in determining the expansion pattern.

摘要

气候变化对日本北部白纹伊蚊(Skuse)分布的影响进行了分析,由于该地区的时间序列分布记录不完整。我们分析了当地气候数据,使用蚊子热适宜指数(TSI)和年平均温度作为时间的线性回归。在日本北部,自 20 世纪初以来,热条件对白纹伊蚊变得越来越适宜,这主要是由于越冬季节的寒冷程度降低,而繁殖季节的温暖程度增加。基于白纹伊蚊在北部边界范围的最近发现记录,我们确定了估计其持续建立的热条件的热标准。回顾性分析表明,在 20 世纪 80 年代中期以后的加速升温之前,这些标准在本州北部的大多数沿海低地以及 1990 年以后该物种的第一个记录中都已经达到;在一些地点,温度标准在 20 世纪初或之前已经达到。1990 年后,热适宜范围的扩大仅在内陆地区和最北部的太平洋海岸得到支持。估计的扩展速度约为每十年 26 公里。我们的分析还表明,局部气候异质性(除了南北或海拔温度梯度)在确定扩展模式方面的重要性。

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