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Investigating Coral Reef Loss and Its Causes around Panggang Island, Seribu Islands, Indonesia

机译:调查珊瑚礁损失及其在庞格岛,Seribu岛,印度尼西亚

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The growth of coral reefs is influenced by two factors that are natural and anthropogenic factors, which natural factor include salinity, temperature, light and solar radiation, nutrients, and depth. The objective of this study was to examine the changes in coral reefs area around Panggang Island and to know: whether oceanographic parameters such as temperature, chlorophyll-a, salinity. pH. brightness, hotspots, thermal stress. El Nino Southern Oscillation (ENSO). and Indian Ocean Dipole (lOD) influence the change. The method used in this research is remote sensing and field data observation. The image data used comes from Landsat 7 ETIVT (2001-2003) and Landsat 8 OLI / TIRS (2013-2016) for coral reefs. NOAA Coral Reef Watch Satellite Monitoring data (2013-2016) for Sea Surface Temperature (SST) and Aqua Modis data (2002-2003 and 2013-2016) for chlorophyll-a. Field data for seawater quality in April 2016 obtained from National Institute of Aeronautics and Space. Meanwhile. Ocean Nino Index and Dipole Mode Index downloaded from Jamstee and NOAA websites. The results showed that the average rate loss of coral reefs area around Panggang Island, during 2001-2016 is 10.74 ha /year. The highest coral reef loss occurs in the 2013-2014 (42.9 ha), this is due to thermal stress in December 2013 to April 2014 which reached -2.25°C / week. In 2014-2015 the coral reef area is increase by 37.3 ha. this is due to the coral planting activities in the study area. During 2013-2016 there is only one hotspot. so the phenomenon does not affect the change of coral width. ENSO and IOD didn't seem to affects the coral reef loss in the study area. According to field observation in April 2016. the parameters that meet the reef growth standards are chlorophyll-a and pH, while temperature, salinity, and brightness does not meet the coral reef standards.
机译:珊瑚礁的生长受到自然和人为因素的两个因素的影响,自然因素包括盐度,温度,光和太阳辐射,营养素和深度。本研究的目的是检查Panggang Island周围的珊瑚礁区域的变化,并知道:温度,叶绿素-A,盐度等海洋参数。 pH。亮度,热点,热应力。 El Nino Southern振荡(ENSO)。和印度洋偶极子(LOD)影响变化。本研究中使用的方法是遥感和现场数据观察。使用的图像数据来自Landsat 7 Etivt(2001-2003)和Landsat 8 Oli / Tirs(2013-2016)用于珊瑚礁。 Noaa Coral Reef手表卫星监测数据(2013-2016),用于海面温度(SST)和Aqua Modis数据(2002-2003和2013-2016),用于叶绿素-A。 2016年4月的海水质量现场数据从国家航空航天研究所获得。同时。 Ocean Nino索引和偶极模式指数从Jamstee和Noaa网站下载。结果表明,2001 - 2016年期间,Panggang Island珊瑚礁区的平均速率损失为10.74公顷。最高珊瑚礁损失发生在2013 - 2014年(42.9公顷)中,这是由于2013年12月至2014年4月的热力压力,达到-2.25°C /周。 2014 - 2015年,珊瑚礁面积增加37.3公顷。这是由于研究区域的珊瑚种植活动。 2013 - 2016年期间只有一个热点。因此,现象不会影响珊瑚宽度的变化。 ENSO和IOD似乎没有影响研究区域的珊瑚礁损失。根据2016年4月的野外观察。满足Reef生长标准的参数是叶绿素-A和pH,而温度,盐度和亮度不符合珊瑚礁标准。

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