首页> 外文会议>Dragon 3 Final Results amp; Dragon 4 Kick-Off Symposium >CONCERTED EARTH OBSERVATION AND PREDICTION OF WATER AND ENERGY CYCLES IN THE THIRD POLE ENVIRONMENT (CEOP-TPE)
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CONCERTED EARTH OBSERVATION AND PREDICTION OF WATER AND ENERGY CYCLES IN THE THIRD POLE ENVIRONMENT (CEOP-TPE)

机译:第三极环境(CEOP-TPE)中的地球观测和水和能源循环的预测

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摘要

The achievements made in Dragon III in 2014-2016 are listed below:rn1. Maintaining the Tibetan Plateau Soil Moisture and Soil Temperature Observatory (Tibet-Obs) [1-3] and developing a method and data product by blending SM product over Tibetan Plateau and evaluating other available SM products [4].rn2. Developing a new algorithm for representing the effective soil temperature in microwave radiometry [5-7].rn3. Developing data sets to study the regional and plateau scale land-atmosphere interactions in TPE [8-11].rn4. Identifying and developing improved land surface processes [12-15].rn5. Developing a method for the quantification of water cycle components based on earth observation data and a comparison to reanalysis data [16-17].rn6. Investigating and revealing the mechanism of surface and tropospheric heatings on the Tibetan plateau [18].rn7. Proposing a validation framework for the generation of climate data records [19].rn8. Graduating seven young scientists with their doctorates during the last two years of Dragon III programme.rn9. Making the datasets and algorithms accessible to the scientific community.
机译:2014-2016年《龙腾三世》取得的成就如下:rn1。维持青藏​​高原土壤水分和土壤温度观测站(1-3),并通过在青藏高原上混合SM产品并评估其他可用的SM产品来开发方法和数据产品[4] .rn2。开发一种用于表示微波辐射法中有效土壤温度的新算法[5-7] .rn3。开发数据集以研究TPE中区域和高原规模的陆地-大气相互作用[8-11] .rn4。确定和开发改进的陆地表面过程[12-15] .rn5。开发一种基于地球观测数据并将其与再分析数据进行比较的水循环成分定量方法[16-17] .rn6。研究和揭示青藏高原地表和对流层加热的机理[18] .rn7。提出用于生成气候数据记录的验证框架[19] .rn8。在Dragon III计划的最后两年中,有七名年轻的科学家和博士学位毕业。使数据集和算法可供科学界使用。

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  • 会议地点 Wuhan(CN)
  • 作者单位

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands, email: z.su@utwente.nl;

    Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;

    Technical University of Delft, The Netherlands;

    Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China;

    Universitat de Valencia, Spain;

    National Meteorological Center, Beijing, China;

    Institute of Geographic Sciences and Natural Resources Research, Beijing, China;

    Institute of Geographic Sciences and Natural Resources Research, Beijing, China;

    University of Stuttgart, Germany;

    China University of Science and Technology, Hefei, China;

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands;

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands;

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands;

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands;

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands;

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands;

    Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands;

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