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Seasonal variation of UV radiation in the ocean under clear and cloudy conditions

机译:在晴朗和多云的条件下,海洋中紫外线辐射的季节性变化

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Seasonal variability of solar UV radiation in ocean waters is estimated on a global scale by combining satellite measurements of scene reflectivity (TOMS), column ozone (TOMS) and chlorophyll concentration (SeaWiFS) with radiative transfer calculations for an ocean-atmosphere system. The new features are an extension of underwater radiative transfer (scattering and absorption) into the UV, inclusion of polarization in the above water diffuse radiances, the proper treatment of Fresnel reflection, and first order atmospheric backscatter of water-leaving radiance to the oceans. Maps of downwelling diffuse irradiances (E_d) at ocean surface and at different depths in the ocean, diffuse attenuation coefficient (K_d), and ten percent penetration depth (Z_(10)) of solar irradiation are computed for open ocean waters. Results on spectral irradiances at 310 nm in UV-B and at 380 nm in UV-A part of the spectrum are presented with particular emphasis on the role of aerosols, clouds, and ozone in the atmosphere and chlorophyll concentrations in the ocean.
机译:通过结合对场景反射率(TOMS),柱状臭氧(TOMS)和叶绿素浓度(SeaWiFS)的卫星测量结果与海洋-大气系统的辐射转移计算相结合,可以估算全球海水中太阳紫外线辐射的季节性变化。这些新功能包括将水下辐射转移(散射和吸收)扩展到紫外线,在上述水扩散辐射中包括极化,适当处理菲涅耳反射以及将水辐射向海洋的一级大气反向散射。对于开阔的海水,计算了海面和海洋不同深度处的向下扩散漫射辐射(E_d),漫射衰减系数(K_d)和太阳辐射的百分之十渗透深度(Z_(10))的地图。给出了UV-B在310 nm和UV-A在380 nm处的光谱辐照度的结果,特别着重于大气中的气溶胶,云和臭氧的作用以及海洋中叶绿素的浓度。

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