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100/11/16

()

15:3017:00

中央大學科學二館S1-713教室

Prof. Shuanggen Jin

金双根 教授

Shanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai, China.

GNSS Remote Sensing: Recent results and Challenges

100/11/16

()

14:0015:00

中央大學科學二館S1-713教室

鍾高陞 博士

Data Assimilation and Satellite Meteorology Research Section Science & Technology Branch, Environment Canada

Transition to flow dependent background error covariances at the convective scale in the context of the Ensemble Kalman Filter

100/11/16

()

11:2012:10

台大大氣A100教室

Prof. Xin-Zhong Liang

Department of Atmospheric & Oceanic Science and

Earth System Science Interdisciplinary Center

University of Maryland, USA

Regional Climate-Weather Research and Forecasting (CWRF) Model Development and Application for Precipitation Prediction

吳俊傑

台大大氣系

100/11/16

() new

10:3011:30

中央研究院環變中心演講廳(人文館南棟11)

Prof. Chi-Kuei Wang

王驥魁 助理教授

成功大學測量及空間資訊學系

High Density Airborne LiDAR Data for Instream Flow Type Mapping

100/11/15

()

16:0017:00

中央大學科學二館S1-713教室

Prof. Xin-Zhong Liang

Department of Atmospheric & Oceanic Science and

Earth System Science Interdisciplinary Center

University of Maryland, USA

A Regional Model for Studies on Taiwan Climate

100/11/15

()

15:0016:00

中央大學科學二館S1-713教室

柯亙重 教授

高雄師範大學地理系

The sub-monthly wave pattern and the associated recurving tropical cyclones during the extreme ISO phases in the tropical western North Pacific

100/11/15

() new

14:0015:00

中央大學科學一館S-325教室

曾若玄 教授

中山大學海洋生物科技暨資源學系

Measurements of turbulent mixing in the surrounding waters of Taiwan

100/11/14

()

15:3016:20

台大大氣A100教室

鍾高陞 博士

Data Assimilation and Satellite Meteorology Research Section Science & Technology Branch, Environment Canada

Transition to flow dependent background error covariances at the convective

scale in the context of the Ensemble Kalman Filter

吳俊傑

台大大氣系

100/11/14

()

14:0016:00

中央氣象局 4樓視訊室

Prof. Russell L. Elsberry

Naval Postgraduate School

USA

Tropical Cyclone Formation and Rapid Intensity Changes-Environmental Control versus Mesoscale/ Convective Scale Processes

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