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Underwater Optics in Sub-Antarctic and Antarctic Coastal Ecosystems

机译:南极和南极沿海生态系统的水下光学

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摘要

Understanding underwater optics in natural waters is essential in evaluating aquatic primary production and risk of UV exposure in aquatic habitats. Changing environmental conditions related with global climate change, which imply potential contrasting changes in underwater light climate further emphasize the need to gain insights into patterns related with underwater optics for more accurate future predictions. The present study evaluated penetration of solar radiation in six sub-Antarctic estuaries and fjords in Chilean North Patagonian region (39–44°S) and in an Antarctic bay (62°S). Based on vertical diffuse attenuation coefficients (Kd), derived from measurements with a submersible multichannel radiometer, average summer UV penetration depth (z1%) in these water bodies ranged 2–11 m for UV-B (313 nm), 4–27 m for UV-A (395 nm), and 7–30 m for PAR (euphotic zone). UV attenuation was strongest in the shallow Quempillén estuary, while Fildes Bay (Antarctica) exhibited the highest transparency. Optically non-homogeneous water layers and seasonal variation in transparency (lower in winter) characterized Comau Fjord and Puyuhuapi Channel. In general, multivariate analysis based on Kd values of UV and PAR wavelengths discriminated strongly Quempillén estuary and Puyuhuapi Channel from other study sites. Spatial (horizontal) variation within the estuary of Valdivia river reflected stronger attenuation in zones receiving river impact, while within Fildes Bay a lower spatial variation in water transparency could in general be related to closeness of glaciers, likely due to increased turbidity through ice-driven processes. Higher transparency and deeper UV-B penetration in proportion to UV-A/visible wavelengths observed in Fildes Bay suggests a higher risk for Antarctic ecosystems reflected by e.g. altered UV-B damage vs. photorepair under UV-A/PAR. Considering that damage repair processes often slow down under cool temperatures, adverse UV impact could be further exacerbated by cold temperatures in this location, together with episodes of ozone depletion. Overall, the results emphasize the marked spatial (horizontal and vertical) and temporal heterogeneity of optical characteristics, and challenges that these imply for estimations of underwater optics.
机译:了解天然水中的水下光学器件对于评估水生初级产品和水生生境中紫外线暴露的风险至关重要。与全球气候变化有关的不断变化的环境条件,暗示着水下光气候的潜在对比变化,进一步强调了需要深入了解与水下光学器件有关的模式,以进行更准确的未来预测。本研究评估了智利北巴塔哥尼亚地区(39-44°S)和南极湾(62°S)的六个南极亚河口和峡湾的太阳辐射穿透力。根据使用潜水式多通道辐射计的测量结果得出的垂直扩散衰减系数(Kd),这些水体中的夏季平均紫外线穿透深度(z1%)对于UV-B(313 nm)为4–27 m,范围为2–11 m对于UV-A(395 nm),对于PAR(共沸区)为7–30 m。在浅色的Quempillén河口,紫外线衰减最强,而菲尔德斯湾(南极洲)则表现出最高的透明度。光学上非均质的水层和透明度的季节性变化(冬季较低)是科莫峡湾和普玉花皮航道的特征。通常,基于UV和PAR波长的Kd值进行的多变量分析将Quempillén河口和Puyuhuapi河道与其他研究地点区分开来。瓦尔迪维亚河河口内的空间(水平)变化反映出受河冲刷的区域衰减加剧,而在菲尔德斯湾内,较低的水透明度空间变化通常可能与冰川的密闭性有关,这可能是由于冰驱动引起的浊度增加流程。与Fildes湾中观察到的UV-A /可见波长成比例的更高的透明度和更深的UV-B穿透率表明,南极生态系统的风险更高,例如在UV-A / PAR下改变了UV-B损伤与光修复。考虑到损坏修复过程通常在低温下会变慢,因此该位置的低温以及臭氧消耗的情况可能会进一步加剧不利的紫外线影响。总体而言,结果强调了光学特性在空间(水平和垂直)和时间上的异质性,并暗示了这些挑战对水下光学器件的估计。

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