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Gabriëlle J. M. De Lannoy, Rolf H. Reichle, and Valentijn R. N. Pauwels

the daily updated data (processing versions SCLF1C 504 and 505 and SMUDP2 500 and 551) distributed by the European Space Agency. The preprocessing of the SMOS observations for use in the present study involves several steps. First, we collect all antenna-level SMOS SCLF1C Tb observations for a given grid cell and half orbit. We then apply a quality control to their angular signature by eliminating observations that fall outside of a one-standard-deviation range around the 5° angular moving average

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Haolu Shang, Li Jia, and Massimo Menenti

exploiting Dragon time series and field measurements. Proc. Dragon 2 Final Results and Dragon 3 Kick-Off Symp., Beijing, China, Ministry of Science and Technology of China and European Space Agency, CD-ROM . Jia, L. , Shang H. , Hu G. , and Menenti M. , 2011 : Phenological response of vegetation to upstream river flow in the Heihe Rive basin by time series analysis of MODIS data . Hydrol. Earth Syst. Sci. , 15 , 1047 – 1064 , doi: 10.5194/hess-15-1047-2011 . Julien, Y. , Sobrino J. A

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Junchao Shi, Massimo Menenti, and Roderik Lindenbergh

mountainous areas. This means that satellite full-waveform laser altimetry is a new capable way to derive basic elements (the terrain irregularities) of the energy exchange process in the ABL of remote areas in the Tibetan Plateau and similar mountainous regions on Earth. Acknowledgments This research was founded by the European Commission (Call FP7-ENV-2007-1 Grant 212921) as part of the CEOP-AEGIS project. We thank NASA's ICESat Science Project and the NSIDC for distribution of the ICESat data, the

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Donghai Zheng, Rogier van der Velde, Zhongbo Su, Martijn J. Booij, Arjen Y. Hoekstra, and Jun Wen

) . Acknowledgments This research was funded in part by the ESA-MOST Dragon I/II program (Drought Monitoring, Prediction and Adaptation under Climatic Changes project and Young Scientists Support), the European Commission CEOP–AEGIS project (Call FP7-ENV-2007-1 Grant 212921; http://www.ceop-aegis.org/ ), and the ESA STSE WACMOS project ( www.wacmos.org ). Donghai Zheng is supported by Chinese Scholarship Council (CSC). The authors thank Professor Jun Wen in CAREERI/CAS for providing the field observations

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Mustafa Gokmen, Zoltan Vekerdy, Maciek W. Lubczynski, Joris Timmermans, Okke Batelaan, and Wouter Verhoef

respect to instantaneous and daily air temperature, the local lapse rates were calculated for the mountainous areas and integrated (based on a DEM) in the interpolation of air temperature data. Finally, the downwelling shortwave and longwave radiation flux ( R swd and R lwd ), boundary layer height, and dewpoint temperature at 2-m height were retrieved from the high-resolution gridded European Centre for Medium-Range Weather Forecasts (ECMWF) Interim Re-Analysis (ERA-Interim) dataset ( http

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