Tri Wahyu Hadi
Bandung Institute of Technology
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Featured researches published by Tri Wahyu Hadi.
IOP Conference Series: Earth and Environmental Science | 2017
I Dewa Gede Agung Junnaedhi; Edi Riawan; Rusmawan Suwarman; Tri Wahyu Hadi; Atika Lubis; Nurjanna Joko Trilaksono; Rahmawati Rahayu; PrawiraYudha Kombara; Riki Waskito; Hendra Ekalaya Oktora; Rahmat Supriatna; Aan Anugrah; Abdul Haq Mudzakkir; Wawar Setiawan
Majalaya, a small city to the south-east of Bandung, was hit by flood almost every year. From January to June 2016, up to 5 severe floods and 4 moderate floods have hit this city. Although it usually not last for long, but the flood stream could be very rapid, thus have a high potential to bring damage to the city. Starting from 2012, ITB through Weather and Climate Prediction Laboratory (WCPL) has support Garda Caah (flood watcher society in Majalaya) with weather prediction system. In the late 2015, ITB also enhancing Garda Caah observation system by installing several Automatic Weather Station (AWS) and Automatic Water Level Recorder (AWLR) throughout Majalaya upstream area. The instruments itself was supported by a re-insurance company MAIPARK and some was built in house by WCPL. The collaboration between ITB, Garda Caah, and Majalaya citizens has been proved to be mutually beneficial. Garda Caah could get more accurate and faster observation and enhanced knowledge, thus could provide a better flood warning for Majalaya citizens. On the other hand, ITB could get data from observation network, with more efficient way to maintain observation instruments as it done by Garda Caah and other Majalaya citizens.
INTERNATIONAL SYMPOSIUM ON EARTH HAZARD AND DISASTER MITIGATION (ISEDM) 2016: The 6th Annual Symposium on Earthquake and Related Geohazard Research for Disaster Risk Reduction | 2017
Aditia Rojali; Abdul Somat Budiaji; Yudhistira Satya Pribadi; Dita Fatria; Tri Wahyu Hadi
This paper addresses on the numerical modeling approaches for flood inundation in urban areas. Decisive strategy to choose between 1D, 2D or even a hybrid 1D-2D model is more than important to optimize flood inundation analyses. To find cost effective yet robust and accurate model has been our priority and motivation in the absence of available High Performance Computing facilities. The application of 1D, 1D/2D and full 2D modeling approach to river flood study in Jakarta Ciliwung river basin, and a comparison of approaches benchmarked for the inundation study are presented. This study demonstrate the successful use of 1D/2D and 2D system to model Jakarta Ciliwung river basin in terms of inundation results and computational aspect. The findings of the study provide an interesting comparison between modeling approaches, HEC-RAS 1D, 1D-2D, 2D, and ANUGA when benchmarked to the Manggarai water level measurement.
Journal of Physics: Conference Series | 2016
Rattana Chhin; Nurjanna Joko Trilaksono; Tri Wahyu Hadi
Indochina Peninsula is located in between Bay of Bengal (BoB) and South-China Sea (SCS). This region is affected frequently from Tropical Cyclones (TCs) formed in North Indian Ocean (NIO), South-China Sea (SCS), and North West Pacific Ocean (NWP). This research analyzed the structure of the rainfall over Indochina Peninsula and its relationships with TCs from the aforementioned sources. Principle Component Analysis (PCA) was performed to investigate the dominant rainfall area produced from those TCs. Spatial and Temporal structures of rainfall from the TCs is analyzed to understand their propagation. The results show that the dominant TC rainfall area covers Central Vietnam which contributed around 25% to total rainfall in the region. However, the contribution of this TC rainfall over LMB is likely less than 20% where Laoss territory receives highest contribution (20%). Furthermore, from the three source areas, TCs formed in SCS produce the highest rain rate when they develop into typhoon intensity stage of Joint Typhoon Warning Center (JTWC)s scale. The average duration of TC rainfall over Indochina Peninsula is 81.28 hours, and over LMB is 66.22 hours. Thus, same as other regions in the Indochina Peninsula, LMB is affected by TC rainfall with considerable scales both spatially and temporally that may lead to significant hydrometeorological hazards.
Theoretical and Applied Climatology | 2015
Elza Surmaini; Tri Wahyu Hadi; Kasdi Subagyono; Nanang T. Puspito
Archive | 2009
Djoko Santoso Abi Suroso; Tri Wahyu Hadi; Ibnu Sofian; Hamzah Latief; Oman Abdurahman; Budhi Setiawan
Sola | 2016
Trismidianto; Tri Wahyu Hadi; Sachinobu Ishida; Qoosaku Moteki; Atsuyoshi Manda; Satoshi Iizuka
Indonesian Journal of Agricultural Science | 2015
Elza Surmaini; Tri Wahyu Hadi; Kasdi Subagyono; Nanang T. Puspito
Jurnal Meteorologi dan Geofisika | 2012
Indra Gustari; Tri Wahyu Hadi; Safwan Hadi; Findy Renggono
京都大学防災研究所年報. B = Disaster Prevention Research Institute annuals. B | 2006
Palikone Thalongsengchanh; Tri Wahyu Hadi; Masanori Niwano; Shigenori Otsuka; Shigeo Yoden
MATEC Web of Conferences | 2018
Edi Riawan; Tri Wahyu Hadi; Hadi Kardhana; Dadang Kurniadi Mihardja; Benyamin Sapiie