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A modern concept for autonomous and continuous measurements of spectral albedo and transmittance of sea ice

机译:自主和连续测量光谱反照率和海冰透射率的现代概念

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Time series of irradiance data measured on sea ice with high temporal and spectral resolution are needed for advancing studies of atmosphere-ice-ocean interaction during different seasons. In particular, more observations of under-ice irradiance are needed to quantify fluxes through snow and sea ice and their seasonality, because the vertical and spectral partitioning of solar radiation are still among the biggest unknowns in today's descriptions of sea-ice related processes. Our current understanding of the interaction of radiation and sea ice is based on only a few data sets, yet this interaction is crucial for describing such processes as sea-ice formation, snow metamorphism, and snow and ice melt, as well as biological productivity and abundance. A modern setup for synchronous, autonomous, continuous, and high temporal-resolution measurements of spectral albedo and transmittance of sea ice is presented. The setup is based on three spectral radiometers, covering a wavelength range from 320 to 950 nm with 3.3 nm spectral resolution. Sensors, data logger, and their setup have worked well in several campaigns under challenging climatic conditions. The longest campaign lasted more than 4 months, without the need for maintenance, and the sensors have shown good performance related to surface contamination, one of the most challenging aspects for radiation measurements. Measured data are of high quality, including details of spectral shapes and high sensitivity to changes in observed snow and ice conditions. All spectra are calibrated for absolute readings, allowing applications in a wide variety of snow and ice studies and their comparison. A sample data set, collected over two weeks in the central Arctic, is presented and shows how the vertical partitioning of irradiance changes during the transition from summer to autumn. The main advantage of the system is its suitability for autonomous and long-term observations over and under sea ice. Furthermore, the setup is portable and robust, and can be easily and quickly installed, which is most valuable for deployment under harsh conditions and also encourages short observation periods. Spectral range and other technical features permit the application of this setup for various interdisciplinary studies, too.
机译:为了进一步研究不同季节的大气-冰-海相互作用,需要在海冰上测量到的具有高时间和光谱分辨率的辐照数据的时间序列。特别是,需要更多的冰底辐照度观测来量化通过雪和海冰的通量及其季节变化,因为在当今关于海冰相关过程的描述中,太阳辐射的垂直和光谱划分仍然是最大的未知数。我们目前对辐射与海冰相互作用的理解仅基于少数数据集,但是这种相互作用对于描述海冰形成,雪变质,雪冰融化以及生物生产力和丰富。提出了一种现代的同步,自主,连续和高时间分辨率光谱反照率和海冰透射率测量装置。该设置基于三个光谱辐射计,覆盖了320至950 nm的波长范围,光谱分辨率为3.3 nm。在挑战性的气候条件下,传感器,数据记录器及其设置在许多活动中都运行良好。最长的活动持续了超过4个月,无需维护,并且传感器表现出与表面污染相关的良好性能,这是辐射测量最具挑战性的方面之一。测得的数据质量很高,包括光谱形状的详细信息以及对观测到的冰雪状况变化的高度敏感性。所有光谱均经过校准以获取绝对读数,从而可用于各种冰雪研究及其比较。展示了在北极中部两周内收集的一个样本数据集,该数据集显示了从夏季到秋季过渡期间辐照度的垂直分区是如何变化的。该系统的主要优点是适用于在海冰之上和之下进行自主和长期观测。此外,该装置具有便携性和鲁棒性,并且可以轻松,快速地安装,这对于在恶劣条件下进行部署最有价值,并且还可以缩短观察周期。光谱范围和其他技术特征也允许将该设置应用于各种跨学科研究。

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