Cantarell natural seep modelling using SAR derived ocean surface wind and meteo- oceanographic buoy data.

机译：Cantarell Natural Seep建模使用SAR衍生的海洋表面风和Meteo-海洋浮标数据。

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The Cantarell Seep is the most significant natural seep discovered in the Southern Gulf of Mexico. The trajectory of the oil seep, driven by sea surface winds and ocean currents, can sometimes impinge on the environmentally sensitive Mexican coast. For this reason it is necessary for the implementation of slick impact models to determine and track oil slick behaviour on sea surface as an aid to contingency planning. The focus of this study was to improve the confidence of the Cantarell natural seep impact model by utilizing SAR derived ocean surface wind field data and in situ meteo-oceanographic buoy data. The advantage of the SAR wind is that the data provides high resolution, wide-area coverage, up to 500 km by 500 km in the case of RADARSAT-1. The accuracies are +/− 2 m/s for wind speed and +/− 25° for wind direction. The buoy is stationary and only provides wind data for that location but the instruments are more sensitive and provide higher accuracies than the SAR. The buoy information is recorded in one-minute intervals, transmitted to shore by microwave communication and the accuracies are +/− 0.7 m/s for wind speed and +/−3° for wind direction. Our approach was to combine the two data sources to provide better coverage and accuracy for oil slick modeling.

机译：Cantarell Seep是墨西哥南部最重要的自然席席。由海表面风和海洋电流驱动的石油渗透的轨迹有时可以在环保敏感的墨西哥海岸上冲击。因此，有必要实施光滑的影响模型，以确定海面上的油烟行为作为应急计划的援助。本研究的重点是通过利用SAR衍生的海洋风场数据和原位地海洋浮标数据来提高Cantarell天然渗透冲击模型的置信度。 SAR风的优势在于数据提供高分辨率，广域覆盖率，在雷达拉-1的情况下，高达500 km达500公里。用于风速的准确度为+/- 2米/秒，风向为+/- 25°。浮标是静止的，只为该位置提供风数据，但仪器更敏感并提供比SAR更高的精度。浮标信息以一分钟的间隔记录，通过微波通信传输到岸边，对于风速，精度为+/- 0.7米/秒，风向为+/- 3°。我们的方法是结合两种数据来源，为油光滑建模提供更好的覆盖率和准确性。

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《IEEE International Geoscience and Remote Sensing Symposium》|2007年||共4页
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作者
Herrera Rodriguez Miguel; Bannerman Karen; Gomez Caceres Ricardo; Pellon de Miranda Fernando; Campos Pedroso Enrico; IGARSS;
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中图分类 P3-53;
关键词
SAR images; oil slick; slick impact models;

机译：SAR图像;油幻灯片;光滑的影响模型;

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1. Evaluation of Oceansat-2-Derived Ocean Surface Winds Using Observations From Global Buoys and Other Scatterometers [J] . Kumar R., Chakraborty A., Parekh A., Geoscience and Remote Sensing, IEEE Transactions on . 2013,第5期

机译：使用全球浮标和其他散射仪的观测结果评估Oceansat-2衍生的海洋表面风
2. Comparison of Ocean Surface Winds From ENVISAT ASAR, MetOp ASCAT Scatterometer, Buoy Measurements, and NOGAPS Model [J] . Xiaofeng Yang, Xiaofeng Li, Pichel W.G., Geoscience and Remote Sensing, IEEE Transactions on . 2011,第12期

机译：ENVISAT ASAR，MetOp ASCAT散射仪，浮标测量和NOGAPS模型对海洋表面风的比较
3. Application of satellite-derived ocean surface winds to the detection of weather systems and the prediction of near-ocean surface winds around Hawaii [J] . Yeh H.-C. TAO: Terrastrial, atmospheric, and oceanic sciences . 2010,第6期

机译：卫星海面风在气象系统探测和夏威夷周围近海海面风的预测中的应用
4. Cantarell natural seep modelling using SAR derived ocean surface wind and meteo- oceanographic buoy data. [C] . Herrera Rodriguez Miguel, Bannerman Karen, Gomez Caceres Ricardo, IEEE International Geoscience and Remote Sensing Symposium . 2007

机译：Cantarell Natural Seep建模使用SAR衍生的海洋表面风和Meteo-海洋浮标数据。
5. System design of a high data rate oceanographic telemetry buoy. [D] . Clark, Andrew Malcolm. 1995

机译：高数据速率海洋遥测浮标的系统设计。
6. Path Optimization along Buoys Based on the Shortest Path Tree with Uncertain Atmospheric and Oceanographic Data [O] . Han Xue, Tian Chai 2021

机译：基于浮标的路径优化基于不确定的大气和海洋数据的最短路径树
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。
8. Applicability of National Data Buoy Systems to Refined National Requirements for Marine Meteorological and Oceanographic Data. Volume II: Appendixes [R] . Clem, L. H., Northrop, G. M. 1968

机译：国家数据浮标系统对海洋气象和海洋数据精确国家要求的适用性。第二卷：附录

Cantarell natural seep modelling using SAR derived ocean surface wind and meteo- oceanographic buoy data.

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