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Decadal changes in sea surface temperature, wave forces and intertidal structure in New Zealand

机译:新西兰海面温度,波浪力和潮间带结构的年代际变化

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Predictions of the effects of climate change in the coastal zone require an understanding of the relationships between environmental and biotic variables. These are often highly complex and uncertain because of the many ways marine biota interact with each other under different environmental conditions. We use data collected over the past several decades to determine changes in the key environmental variables and area-specific changes in the dominant habitat-forming macroalgae. Sea surface temperature (SST) data and wave heights from ERA-Interim reanalysis were analysed for 3 areas of the east coast of New Zealand's South Island to detect trends over the past 30 yr. We then used detailed benthic survey data acquired quarterly or half-yearly in 2 tidal zones at the same coastal areas from 1994 onwards. There were significant increases in the mean SST at 2 of the 3 areas, with average increases of 0.16 degrees C per decade over 3 decades. Maximum SST did not increase, but the minimum seawater temperatures did, by up to 0.34 degrees C per decade. Mean significant wave height also increased over this period by 0.06 m per decade, and maximum wave height by up to 0.3 m per decade at 2 of the 3 areas. Boosted regression tree analysis was used to determine any consistent patterns between physical variables and benthic algal cover. Generally, air temperature and the Southern Oscillation Index (SOI) were the most influential variables on cover of fucoid macroalgae. SST and wave height were also important but less influential. Fucoid cover increased with maximum air temperature beyond ca. 22 to 24 degrees C, and cover decreased during La Nina periods at the most northern site, but increased during La Nina periods at the most southern site. The relative contributions of SST and wave height variables to the models were area- and tidal zone-specific. Overall, this study showed highly variable effects of a changing climate on an ecologically important habitat-former, highlighting the problems of dealing with ecological and climate variables that operate at differing spatial and temporal scales. We discuss this with respect to community structure and dynamics.
机译:预测沿海地区气候变化的影响需要了解环境和生物变量之间的关系。由于海洋生物在不同的环境条件下相互影响的方式很多,因此它们通常是高度复杂且不确定的。我们使用过去几十年收集的数据来确定主要环境变量的变化以及形成栖息地的主要藻类在特定区域的变化。对ERA临时分析的海表温度(SST)数据和波高进行了分析,分析了新西兰南岛东海岸的3个区域,以发现过去30年的趋势。然后,我们使用了从1994年开始每季度或半年在同一沿海地区的2个潮汐带采集的详细底栖调查数据。 3个区域中有2个区域的平均SST显着增加,在3年中,每10年平均增加0.16摄氏度。最高SST没有增加,但是最低海水温度却增加了,每十年最高增加0.34摄氏度。在此期间,平均有效波高每10年增加0.06 m,在3个区域中的2个区域,最大波高每10年增加0.3 m。使用增强回归树分析来确定物理变量和底栖藻类覆盖之间的任何一致模式。通常,气温和南方涛动指数(SOI)是类岩藻大藻覆盖率影响最大的变量。海面温度和海浪高度也很重要,但影响较小。 Fucoid覆盖物的最高空气温度超过约200摄氏度。在22到24摄氏度之间,最北端的拉尼娜时期覆盖率下降,而最南端的拉尼娜时期覆盖率增加。 SST和波高变量对模型的相对贡献是特定于区域和潮汐带的。总体而言,这项研究显示了气候变化对生态重要的生境形成者的高度可变影响,突出了应对在不同时空尺度上运行的生态和气候变量的问题。我们在社区结构和动态方面对此进行讨论。

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