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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Sea surface temperatures and seagrass mortality in Florida Bay: Spatial and temporal patterns discerned from MODIS and AVHRR data
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Sea surface temperatures and seagrass mortality in Florida Bay: Spatial and temporal patterns discerned from MODIS and AVHRR data

机译:佛罗里达湾的海面温度和海草死亡率:MODIS和AVHRR数据辨别的空间和时间模式

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摘要

Two major episodes of seagrass mortality have occurred in Florida Bay in the past 30 years: The first occurred between 1987 and 1991 and the second began in 2015. In both episodes, dense beds of turtle grass (Thalassia testudinum) were decimated. Elevated water temperature and hypersalinity have been implicated as contributing factors in both mortality events. During both die-off events seagrass beds on shallow (Z approximate to 0.3 m) mudbanks in western Florida Bay were disproportionately affected when compared to neighboring seagrass in deeper basins (Z approximate to 1.5 m). A network of in situ monitoring stations has measured sea surface temperature and salinity at hourly intervals in 16 basins in Florida Bay from August 2009 to the present day and these data aided in diagnosing the 2015-2016 die-off event. However, very few in situ observations of sea surface temperature have been collected on Florida Bay's shallow mudbanks as most are inaccessible by boat. As a result, our understanding of the role of elevated SST in shaping the spatial patterns of seagrass mortality is hindered by the spatial distribution of the in situ monitoring data and its record length. Therefore, we turn to remotely sensed SST data to expand our spatial coverage to include the entire Florida Bay ecosystem and to extend the record length to include the 1987-1991 die-off event. 1 km MODIS SST shows that shallow mudbanks were consistently warmer (by up to 6 degrees C) than nearby deeper basins. While water depth is likely the primary driver of spatial variability in SST, Landsat-8 surface reflectance data suggest that shallow seagrass beds could have suffered from the added influence of low surface reflectance, which might have further contributed to their thermal stress. Daily 0.25 degrees AVHRR SST shows that the August maximum SST has increased by 1 degrees C from 1981 to 2016, which is a cause for concern for the future of seagrass in Florida Bay. Correlation of monthly AVHRR SST ano
机译:在过去的30年里,佛罗里达湾发生了两件大事海湾死亡率:第一次发生在1987年至1991年间,第二次始于2015年。在两次发作,龟草(Thalassia Testudinum)的密集床被抽取。升高的水温和过度高度涉及死亡事件中的贡献因素。在抵消事件中,与邻近盆地(Z近似为1.5米)的邻近的海草相比,佛罗里达湾浅(Z近似为0.3米的Z近似值至0.3米)的海草床。从2009年8月到现在,佛罗里达湾的16个盆地的每小时间隔测量了海面温度和盐度,从2009年8月到现在,这些数据辅助诊断2015-2016模具事件。然而,在佛罗里达湾的浅泥浆中收集了海面温度的原位观察,因为大多数是船只无法进入船只。结果,我们对升高的SST在成形海草死亡率的空间模式的理解是受到原位监测数据的空间分布及其记录长度的阻碍了海草死亡率的空间模式。因此,我们转向远程感知的SST数据,以扩大我们的空间覆盖范围,包括整个佛罗里达湾生态系统,并将记录长度扩展到包括1987-1991芯片熄灭事件。 1 km Modis SST表明,浅泥浆比附近的盆地更温暖(最多6℃)。虽然SST的水深可能是SST的空间变异的主要驱动器,但Landsat-8表面反射率数据表明,浅海草床可能已经遭受了低表面反射率的增加影响,这可能进一步导致其热应力。每日0.25度AVHRR SST表明,8月最高SST从1981年到2016年增加了1摄氏度,这是佛罗里达湾未来对未来的关注的原因。每月AVHRR SST ANO的相关性

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