PROCEEDINGS VOLUME 8529
SPIE ASIA-PACIFIC REMOTE SENSING | 29 OCTOBER - 1 NOVEMBER 2012
Remote Sensing and Modeling of the Atmosphere, Oceans, and Interactions IV
IN THIS VOLUME

0 Sessions, 12 Papers, 0 Presentations
Proceedings Volume 8529 is from: Logo
SPIE ASIA-PACIFIC REMOTE SENSING
29 October - 1 November 2012
Kyoto, Japan
Front Matter: Volume 8529
Proc. SPIE 8529, Front Matter: Volume 8529, 852901 (8 November 2012); doi: 10.1117/12.2016735
Remote Sensing and Modeling I
Proc. SPIE 8529, Precipitation characteristics around Bangladesh revealed by TRMM data, 852902 (8 November 2012); doi: 10.1117/12.976822
Proc. SPIE 8529, Is the simulated increasing trend of dry static stability true or not?, 852904 (8 November 2012); doi: 10.1117/12.977948
Remote Sensing and Modeling II
Proc. SPIE 8529, Satellite-based 3D structure of cloud and aerosols over the Indian Monsoon region: implications for aerosol-cloud interaction, 852907 (8 November 2012); doi: 10.1117/12.979246
Proc. SPIE 8529, Future Doppler lidar wind measurement from space in Japan, 85290A (8 November 2012); doi: 10.1117/12.977283
Remote Sensing and Modeling III
Proc. SPIE 8529, Observing system simulation experiments at Joint Center for Satellite Data Assimilation, 85290B (8 November 2012); doi: 10.1117/12.977561
Proc. SPIE 8529, Impacts of enhanced CCN on the organization of convection and recent reduced counts of monsoon depressions, 85290E (29 November 2012); doi: 10.1117/12.979717
Proc. SPIE 8529, Estimation of regional surface CO2 fluxes with GOSAT observations using two inverse modeling approaches, 85290G (8 November 2012); doi: 10.1117/12.979664
Poster Session
Proc. SPIE 8529, Evaluating the spatial and temporal solar energy potential in South Korea, 85290I (8 November 2012); doi: 10.1117/12.977388
Proc. SPIE 8529, Spatio-temporal variability of drought over northern China and its relationships with Indian-Pacific sea surface temperatures, 85290J (1 July 2013); doi: 10.1117/12.976019
Proc. SPIE 8529, Semi-diurnal variation of surface rainfall studied from global cloud-system resolving model and satellite observations, 85290K (8 November 2012); doi: 10.1117/12.977609
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