{"title":"西南季候风期间斯里兰卡南部沿海水域的上升流现象","authors":"K. Yapa","doi":"10.4038/SLJP.V10I0.3831","DOIUrl":null,"url":null,"abstract":"MODIS (Moderate-resolution Imaging Spectroradiometer) aqua data for 2004 has been used to explore possible coastal upwelling areas around Sri Lanka during southwest monsoon. Two very important ocean parameters, ocean colour and sea surface temperature (SST), derived from MODIS data for the waters surrounding Sri Lanka are studied to understand the variability and the relationship of the two data sets. Remotely sensed data of 1.1 km resolution obtained from MODIS were mapped using seadas software within an area of latitudes between 2.0 N - 13.5 N and longitudes between 72.5 E – 88 E. The days with heavy clouds were excluded. Daily chlorophyll a and SST maps were used to make composites for each week and subsequently for each month. There were between 10 – 20 daily files for each month. The southwest monsoon period arrives roughly in May and generally lasts till September. The chlorophyll concentration varies roughly in the range 0.01 – 10.0 mg m −3 and the sea surface temperature varies between 25 – 32°C in the waters surrounding the island during the year. The monthly composites of chlorophyll a show high productive waters of over 5 mg m −3 average concentration in most of the southern and western coastal ocean during the months of June - August. The sea surface temperature drops by 2 to 3 degrees (centigrade) in coastal ocean waters in the south where high chlorophyll a concentrations are detected. Observation of chlorophyll a and SST maps indicate strong correlation (between 60% - 80% of negative correlation) between the two parameters in the southern coastal ocean region where high chlorophyll a and low SST values are detected in the months of June and July. This may be due to the upwelling phenomenon that occurs in the coastal waters. Upwelling brings cooler nutrient rich waters to the surface enhancing the production of phytoplankton near the surface waters and these high phytoplankton areas are generally attracted by large fish populations. Thus, correct identification of upwelling zones would be highly beneficial in the fishery industry. Key words : MODIS; sea surface chlorophyll a ; SST; southwest monsoon; upwelling DOI: http://dx.doi.org/10.4038/sljp.v10i0.3831 Sri Lanka Journal of Physics, Vol. 10 (2009) 7-15","PeriodicalId":21880,"journal":{"name":"Sri Lankan Journal of Physics","volume":"40 4 1","pages":"7"},"PeriodicalIF":0.0000,"publicationDate":"2009-12-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"14","resultStr":"{\"title\":\"Upwelling phenomena in the southern coastal waters of Sri Lanka during southwest monsoon period as seen from MODIS\",\"authors\":\"K. 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The chlorophyll concentration varies roughly in the range 0.01 – 10.0 mg m −3 and the sea surface temperature varies between 25 – 32°C in the waters surrounding the island during the year. The monthly composites of chlorophyll a show high productive waters of over 5 mg m −3 average concentration in most of the southern and western coastal ocean during the months of June - August. The sea surface temperature drops by 2 to 3 degrees (centigrade) in coastal ocean waters in the south where high chlorophyll a concentrations are detected. Observation of chlorophyll a and SST maps indicate strong correlation (between 60% - 80% of negative correlation) between the two parameters in the southern coastal ocean region where high chlorophyll a and low SST values are detected in the months of June and July. This may be due to the upwelling phenomenon that occurs in the coastal waters. Upwelling brings cooler nutrient rich waters to the surface enhancing the production of phytoplankton near the surface waters and these high phytoplankton areas are generally attracted by large fish populations. Thus, correct identification of upwelling zones would be highly beneficial in the fishery industry. 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引用次数: 14
摘要
2004年的MODIS(中分辨率成像光谱辐射计)水数据用于探索西南季风期间斯里兰卡周围可能的沿海上升流区。研究了两个非常重要的海洋参数,海洋颜色和海表温度(SST),它们来自斯里兰卡周围水域的MODIS数据,以了解这两个数据集的变异性和关系。利用seadas软件在纬度2.0 N ~ 13.5 N,经度72.5 E ~ 88 E范围内对MODIS获得的1.1 km分辨率遥感数据进行制图,排除了重云天气。每日叶绿素a和海表温度图分别用于每周和每月的合成。每个月有10 - 20个每日文件。西南季风期大约在5月到来,通常持续到9月。全年,岛周围海域的叶绿素浓度大致在0.01 - 10.0 mg m - 3之间变化,海面温度在25 - 32°C之间变化。叶绿素a的月复合指数显示,6 - 8月,南部和西部沿海大部分海域的叶绿素a高产水域平均浓度超过5 mg m−3。在检测到高叶绿素a浓度的南部沿海海域,海面温度下降2至3摄氏度。叶绿素a与海表温度图的观测表明,在6、7月叶绿素a高、海表温度低的南部沿海海区,叶绿素a与海表温度具有较强的负相关(60% ~ 80%)。这可能是由于沿海水域出现了上升流现象。上升流将较冷的富含营养的海水带到海面,促进了表层附近浮游植物的生长,而这些浮游植物生长旺盛的地区通常会受到大量鱼类的吸引。因此,正确识别上升流区将对渔业非常有益。关键词:MODIS;海面叶绿素a;风场;西南季风;上升流DOI: http://dx.doi.org/10.4038/sljp.v10i0.3831斯里兰卡物理杂志,Vol. 10 (2009) 7-15
Upwelling phenomena in the southern coastal waters of Sri Lanka during southwest monsoon period as seen from MODIS
MODIS (Moderate-resolution Imaging Spectroradiometer) aqua data for 2004 has been used to explore possible coastal upwelling areas around Sri Lanka during southwest monsoon. Two very important ocean parameters, ocean colour and sea surface temperature (SST), derived from MODIS data for the waters surrounding Sri Lanka are studied to understand the variability and the relationship of the two data sets. Remotely sensed data of 1.1 km resolution obtained from MODIS were mapped using seadas software within an area of latitudes between 2.0 N - 13.5 N and longitudes between 72.5 E – 88 E. The days with heavy clouds were excluded. Daily chlorophyll a and SST maps were used to make composites for each week and subsequently for each month. There were between 10 – 20 daily files for each month. The southwest monsoon period arrives roughly in May and generally lasts till September. The chlorophyll concentration varies roughly in the range 0.01 – 10.0 mg m −3 and the sea surface temperature varies between 25 – 32°C in the waters surrounding the island during the year. The monthly composites of chlorophyll a show high productive waters of over 5 mg m −3 average concentration in most of the southern and western coastal ocean during the months of June - August. The sea surface temperature drops by 2 to 3 degrees (centigrade) in coastal ocean waters in the south where high chlorophyll a concentrations are detected. Observation of chlorophyll a and SST maps indicate strong correlation (between 60% - 80% of negative correlation) between the two parameters in the southern coastal ocean region where high chlorophyll a and low SST values are detected in the months of June and July. This may be due to the upwelling phenomenon that occurs in the coastal waters. Upwelling brings cooler nutrient rich waters to the surface enhancing the production of phytoplankton near the surface waters and these high phytoplankton areas are generally attracted by large fish populations. Thus, correct identification of upwelling zones would be highly beneficial in the fishery industry. Key words : MODIS; sea surface chlorophyll a ; SST; southwest monsoon; upwelling DOI: http://dx.doi.org/10.4038/sljp.v10i0.3831 Sri Lanka Journal of Physics, Vol. 10 (2009) 7-15