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Differential Impact of Anniversary-Severe Cyclones on the Water Quality of a Tropical Coastal Lagoon

机译:周年严重旋风对热带沿海泻湖水质的差异影响

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Mapping spatio-temporal dynamics of suspended load in a lagoon before-during-after a cyclone is crucial for monitoring sudden nutrient enrichment and associated processes such as algal blooms and siltation. However, not all cyclones produce similar impact on a coastal lagoon, some trigger algal blooms after passage while others just increase the overall turbidity. Asia's largest brackish water lagoon, Chilika Lagoon, India was hit by two anniversary-severe cyclones Phailin (12 October 2013) and Hudhud (12 October 2014) recently. Their impacts were analysed with respect to physical, biological and meteorological factors which favour or restrict a phytoplankton bloom after the passage of a storm. Moderate-resolution imaging spectroradiometer surface reflectance data were used to examine the spatio-temporal variability in total suspended sediment (TSS) and chlorophyll-a (Chl-a) concentration pre-and post-cyclone. Comparative results revealed that Phailin was associated with higher rainfall, wind speed and surface runoff compared with Hudhud. These factors contributed to higher TSS concentration in all sectors of the lagoon post-Phailin compared with post-Hudhud. Extreme TSS, limited light, high rainfall and runoff and increased flushing rate post-Phailin restricted the likelihood of a phytoplankton bloom in the lagoon, a commonly reported phenomenon after the passage of a cyclone. In contrast, sufficient light availability due to lower TSS, low runoff and flushing and stable wind supported a phytoplankton bloom post-Hudhud. The observed differential impacts were linked to the individual cyclone's characteristics such as differences in landfall locations, wind speed, trajectory after the landfall, differences in rainfall rate and surface runoff and speed of passage.
机译:在旋风前泻湖中映射悬浮载荷的时空动态,对于监测突然营养丰富和相关过程,如藻类盛开和淤积,这是至关重要的。然而,并非所有旋风都会对沿海泻湖产生类似的影响,在通过后的一些触发藻类绽放,而其他人只是增加整体浊度。亚洲最大的咸水泻湖,奇利卡泻湖,印度北周年严重的克莱林(2013年10月12日)和Hudhud(2014年10月12日)击中。在暴风雨通过后有利于或限制浮游植物盛开的物理,生物和气象因素,分析了它们的影响。适用于中等分辨率的成像光谱致反射率数据来检查总悬浮沉积物(TSS)和叶绿素-A(CHL-A)浓度预先和后旋转后的时空变异性。比较结果表明,与Hudhud相比,Pailin与较高的降雨,风速和表面径流有关。这些因素导致泻湖后帕利诺的所有部门的TSS集中效果与Hudhud后泻湖相比。极端TSS,Limited Light,Rainfall和Runoff,Phailin Pailin的增加率限制了泻湖在泻湖中绽放的可能性,在旋风通道后常见的现象。相比之下,由于较低的TSS,低径流和冲洗和稳定的风而受到充分的光可用性,支持浮游生物绽放后Hudhud。观察到的差异影响与单个旋风分离器的特征有关,例如登陆位置,风速,轨迹在登陆后的差异,降雨率和表面径流差异和通道速度。

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