Measurement of bi-direflectance (BRDF) of sea-ice for Earth Observing Satellites

地球观测卫星海冰双向反射（BRDF）测量

• 批准号: NE/I018999/1
• 负责人: Martin King
• 金额: $ 9.48万
• 依托单位: Royal Holloway University of London
• 依托单位国家: 英国
• 项目类别: Training Grant
• 财政年份: 2011
• 资助国家: 英国
• 起止时间: 2011 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=NE%2FI018999%2F1
• 关键词: Measurement; bi; direflectance; BRDF; sea

The current understanding of climatic influences of black carbon in snow and sea-ice has been described by the intergovernmental panel on climate change, IPCC, to be 'very low' and a better examination of these processes is clearly required. Black carbon from increasing anthropogenic (and biogenic) combustion deposits in polar snow and sea-ice to significantly reduce the reflectivity of the sea-ice or snow. The reduced reflectivity of the Earth surface results in increased warming of the planet. Satellite observations allow for the synoptic observation of large areas of the globe. Remote sensing observations performed in the visible and near infrared (e.g. Meris, MODIS, AVHHR) have wide application in marine, land and snow/ice related climate studies serving as both primary and secondary sources of information. However, although there is significant value in the analysis of data from individual sensors, any global observing system and in particular studies requiring different spatial resolutions and long time bases require accurate knowledge of sensor to sensor biases. This requires the responsivities of all optical radiometers operated in space to be intercompared and traceable to a common reference standard. CEOS (Committee on Earth Observing Satellites) has established a number of Earth targets to serve as international reference standards, each being, or to be, well characterized by surface based in-situ measurements. The reflectance of natural surfaces is not isotropic. The reflectance varies with the illumination and viewing geometries, and consequently impacts satellite observations. Thus the bi-directional reflectance (BRDF) of natural surfaces is a pre-requisite for use of satellite data. Sea-ice is a strong potential calibration target. Working closely with both supervisors the PhD student will generate sea ice in the new RHUL sea-ice simulator. Sea-ice doped with different concentrations of black carbon will be generated in 2000L tanks. The reflectivity of the sea-ice will be measured in the UV and visible parts of the solar spectrum with different zenith and azimuthal angles. The BRDF will be recorded for the sea-ice temperatures of -5 to -25C and black carbon loading of 0-100 ng g(-1). The project will deliver:- (1) A BRDF for sea-ice that can be used by Earth observing satellites to inter-calibrate. This will be delivered to the end users by CASE partner - Dr Nigel Fox, NPL. (2) A BRDF as a function of black carbon content with an assessment of sensitivity of EO satellites to Black carbon loading - i.e. can EO satellites be used to measure BC in sea-ice. (3) Three academic papers reporting the BRDF of seaice as a function of (a) temperature, (b) black carbon concentration, and (c) the sensitivity of BRDF to size, shape, refractive index of the black carbon. The proposed research is low risk, highly rewarding and cost effective and the partnership between Royal Holloway and the NPL is an excellent training opportunity for a PhD student. The applicants have demonstrated in preliminary studies that all experiments are feasible, and have complimentary extensive experience in making BRDF measurements for satellite calibration and measuring the optics of snow and ice. The project is very exciting and highly relevant since it will improve the understanding of black carbon in snow and ice radiative processes. The financial resources required are minimal, RHUL has constructed the sea-ice simulator with CIF money and supported it with a PhD studentship to study ice biogeochemistry. The student will have two fantastic learning environments for this very interdisciplinary project that will directly deliver an important calibration for climate studies by earth observing satellites straight to an end user - i.e. there is clear societal benefit. There is industrial benefit to the UK satellite and Earth observing industry, and end-user is the CASE partner so the project has a real pathway to impact.

政府间气候变化专门委员会(IPCC)将目前对雪和海冰中黑碳的气候影响的理解描述为“非常低”，显然需要对这些过程进行更好的检查。增加极地雪和海冰中人为(和生物)燃烧沉积的黑碳，以显著降低海冰或雪的反射率。地球表面反射率的降低导致了地球变暖的加剧。通过卫星观测，可以对地球大片地区进行天气观测。在可见光和近红外(如MERIS、MODIS、AVHHR)中进行的遥感观测作为主要和次要信息来源，在海洋、陆地和与冰雪有关的气候研究中有着广泛的应用。然而，尽管单个传感器的数据分析具有重大价值，但任何全球观测系统，特别是需要不同空间分辨率和长时间基准的研究，都需要准确了解传感器对传感器的偏差。这要求对在空间运行的所有光学辐射计的响应度进行相互比较，并可追溯到一个共同的参考标准。地球观测卫星委员会(CEOS)制定了若干地球目标作为国际参考标准，每个目标都有或将有很好的地面现场测量的特点。自然表面的反射率不是各向同性的。反射率随照明和观察几何形状的不同而变化，因此影响卫星观测。因此，自然表面的双向反射比(BRDF)是使用卫星数据的先决条件。海冰是一个很有潜力的校准目标。这位博士生将与这两位导师密切合作，在新的RHUL海冰模拟器中产生海冰。在2000L储罐中将产生掺入不同浓度黑碳的海冰。海冰的反射率将在太阳光谱的紫外线和可见光部分以不同的天顶和方位角进行测量。BRDF将记录为海冰温度为-5至-25摄氏度，黑碳负荷量为0-100 ng g(-1)。该项目将提供：-(1)用于海冰的BRDF，可用于地球观测卫星之间的校准。这将由CASE合作伙伴-NPL奈杰尔·福克斯博士交付给最终用户。(2)作为黑碳含量函数的BRDF，并评估EO卫星对黑碳负荷的敏感性--即EO卫星能否用于测量海冰中的BC。(3)三篇学术论文，报道了海冰的BRDF作为(A)温度、(B)黑碳浓度和(C)BRDF对黑碳的大小、形状和折射率的敏感性的函数。拟议的研究是低风险、高回报和高成本效益的，皇家霍洛威与NPL之间的合作对博士生来说是一个极好的培训机会。申请者在初步研究中证明，所有实验都是可行的，并在为卫星校准进行BRDF测量和测量冰雪光学性能方面具有丰富的经验。该项目非常令人兴奋和高度相关，因为它将提高对冰雪辐射过程中黑碳的理解。所需的财政资源很少，RHUL用CIF资金建造了海冰模拟器，并提供了研究冰生物地球化学的博士生奖学金。对于这个非常跨学科的项目，学生将拥有两个极好的学习环境，通过直接向最终用户提供地球观测卫星，直接为气候研究提供重要的校准--即有明显的社会效益。这给英国卫星和地球观测行业带来了产业利益，最终用户是案例合作伙伴，因此该项目有一条真正的影响途径。