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Methods to estimate solar radiation dosimetry in coral reefs using remote sensed, modeled, and in situ data

机译:使用遥感,建模和原地数据估算珊瑚礁太阳辐射剂量的方法

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Solar irradiance has been increasingly recognized as an important determinant of bleaching in coral reefs, but measurements of solar radiation exposure within coral reefs have been relatively limited. Solar radiation dosimetry within multiple coral reef areas of South Florida was assessed using remote sensed, modeled, and measured values during a minor bleaching event during August 2005. Coral reefs in the Dry Tortugas and Upper Keys had similar diffuse downwelling attenuation coefficients (Kd, m~(-1)), whereas Kd values were significantly greater in the Middle and Lower Keys. Mean 1% attenuation depths varied by reef region for ultraviolet B (UVB; 9.7 to 20 m), ultraviolet A (UVA; 22 to 40 m) and visible (27 to 43 m) solar radiation. Solar irradiances determined from remote sensed data were significantly correlated with measured values, but were generally overestimated at the depth of corals. Solar irradiances modeled using an atmospheric radiative transfer model parameterized with site specific approximations of cloud cover showed close agreement with measured values. Estimated daily doses (W h/m~2) of UVB (0.01-19), UVA (2-360) and visible (29-1,653) solar radiation varied with coral depth (2 to 24 m) and meteorological conditions. These results indicate large variation in solar radiation dosimetry within coral reefs that may be estimated with reasonable accuracy using regional Kd measurements and radiative transfer modeling.
机译:太阳辐照度已被越来越多地认为是珊瑚礁褪色的重要决定因素,但是对珊瑚礁内太阳辐射暴露的测量却相对有限。在2005年8月的一次小型漂白事件中,使用遥感,模型化和测量值评估了南佛罗里达州多个珊瑚礁地区的太阳辐射剂量。干龟岛和上礁岛的珊瑚礁具有相似的扩散下降流衰减系数(Kd,m 〜(-1)),而中键和下键的Kd值明显更高。紫外线B(UVB; 9.7至20 m),紫外线A(UVA; 22至40 m)和可见(27至43 m)太阳辐射的平均1%衰减深度随礁区的不同而不同。从遥感数据确定的太阳辐照度与测量值显着相关,但通常在珊瑚深度处被高估了。使用大气辐射传输模型建模的太阳辐照度,该模型使用云量的特定于地点的近似值进行参数化,显示与测量值紧密一致。 UVB(0.01-19),UVA(2-360)和可见光(29-1,653)太阳辐射的估计日剂量(W h / m〜2)随珊瑚深度(2至24 m)和气象条件而变化。这些结果表明,使用区域Kd测量和辐射传递模型可以合理的精度估算珊瑚礁内太阳辐射剂量的巨大变化。

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