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Derivation os the energy balance components using dual angle observations of radiative surface temperature

机译：使用辐射表面温度的双角度观测推导能量平衡分量

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《Geoscience and Remote Sensing Symposium, 2001. IGARSS '01. IEEE 2001 International》|2001年|P.2602-2604|共3页
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Ghani Chehbouni; A.; Nouvelton; Y.; Boulet; G.;
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中图分类无线电电子学、电信技术;
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1. Different approaches in estimating heat flux using dual angle observations of radiative surface temperature [J] . O. MERLIN, A. CHEHBOUNI International journal of remote sensing . 2004,第1期

机译：使用辐射表面温度的双角度观测来估算热通量的不同方法
2. Application of remote sensing-based two-source energy balance model for mapping field surface fluxes with composite and component surface temperatures [J] . Song Lisheng, Liu Shaomin, Kustas William P., Agricultural and Forest Meteorology . 2016,第Null期

机译：基于遥感的两源能量平衡模型在合成和组分表面温度场通量映射中的应用
3. Two-source energy balance model estimates of evapotranspiration using component and composite surface temperatures [J] . Paul D. Colaizzi, William P. Kustas, Martha C. Anderson, Advances in Water Resources . 2012,第DECa期

机译：使用组分和复合物表面温度的蒸散发两源能量平衡模型估算
4. Derivation os the energy balance components using dual angle observations of radiative surface temperature [C] . Ghani Chehbouni, A., Nouvelton, Geoscience and Remote Sensing Symposium, 2001. IGARSS '01. IEEE 2001 International . 2001

机译：使用辐射表面温度的双角度观测推导能量平衡分量
5. Analysis of climate change impacts on surface energy balance of Lake Huron (estimation of surface energy balance components: Remote sensing approach for water -- atmosphere parameterization). [D] . Petchprayoon, Pakorn. 2015

机译：气候变化对休伦湖表面能平衡的影响分析（表面能平衡成分的估算：水-大气参数化的遥感方法）。
6. Estimating Morning Change in Land Surface Temperature from MODIS Day/Night Observations: Applications for Surface Energy Balance Modeling [O] . Christopher R. Hain, Martha C. Anderson -1

机译：根据MODIS日/夜观测值估算地表温度的早晨变化：地表能量平衡模型的应用
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

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