SIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010)

For air transport security, prediction of volcanic ash distribution is needed. The previous study still have shortcomings in predicting this volcanic ash distribution. The previous results of the distribution does not have compatibility with Multifunctional Transport Satellites (MTSAT) satellite ima...

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Main Author: RITDIAWATI PARMANAH (NIM : 12809012); Pembimbing : Dr. Tri Wahyu Hadi , HANA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/18581
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:18581
spelling id-itb.:185812017-09-27T11:45:46ZSIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010) RITDIAWATI PARMANAH (NIM : 12809012); Pembimbing : Dr. Tri Wahyu Hadi , HANA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/18581 For air transport security, prediction of volcanic ash distribution is needed. The previous study still have shortcomings in predicting this volcanic ash distribution. The previous results of the distribution does not have compatibility with Multifunctional Transport Satellites (MTSAT) satellite images for cloudy weather conditions. This is because the previous model did not take into account the vertical velocity of the wind. Vertical velocity is closely related to the process of convection in which the cloud is formed. Therefore, to improve outcomes for ash distribution in cloudy weather, it needs a model volcanic ash distribution that takes into account the distribution of the vertical velocity. FALL3D is one model that takes into the distribution of volcanic ash vertical velocity. FALL3D requires meteorological data input from other models. It use two other meteorological data, the data from the Final Analysis (FNL) global model and data from the atau Weather Research Forecast (WRF) regional model. <br /> <br /> <br /> <br /> <br /> The results of the distribution of volcanic ash WRF using FALL3D model show the suitability with the MTSAT satellite imagery due to the WRF has sufficient horizontal and vertical resolution to predict the phenomenon of cloudy weather. While the FNL nonconformance with the MTSAT satellite imagery since FNL does not have sufficient horizontal and vertical resolution to predict the phenomenon of cloudy weather. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description For air transport security, prediction of volcanic ash distribution is needed. The previous study still have shortcomings in predicting this volcanic ash distribution. The previous results of the distribution does not have compatibility with Multifunctional Transport Satellites (MTSAT) satellite images for cloudy weather conditions. This is because the previous model did not take into account the vertical velocity of the wind. Vertical velocity is closely related to the process of convection in which the cloud is formed. Therefore, to improve outcomes for ash distribution in cloudy weather, it needs a model volcanic ash distribution that takes into account the distribution of the vertical velocity. FALL3D is one model that takes into the distribution of volcanic ash vertical velocity. FALL3D requires meteorological data input from other models. It use two other meteorological data, the data from the Final Analysis (FNL) global model and data from the atau Weather Research Forecast (WRF) regional model. <br /> <br /> <br /> <br /> <br /> The results of the distribution of volcanic ash WRF using FALL3D model show the suitability with the MTSAT satellite imagery due to the WRF has sufficient horizontal and vertical resolution to predict the phenomenon of cloudy weather. While the FNL nonconformance with the MTSAT satellite imagery since FNL does not have sufficient horizontal and vertical resolution to predict the phenomenon of cloudy weather.
format Final Project
author RITDIAWATI PARMANAH (NIM : 12809012); Pembimbing : Dr. Tri Wahyu Hadi , HANA
spellingShingle RITDIAWATI PARMANAH (NIM : 12809012); Pembimbing : Dr. Tri Wahyu Hadi , HANA
SIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010)
author_facet RITDIAWATI PARMANAH (NIM : 12809012); Pembimbing : Dr. Tri Wahyu Hadi , HANA
author_sort RITDIAWATI PARMANAH (NIM : 12809012); Pembimbing : Dr. Tri Wahyu Hadi , HANA
title SIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010)
title_short SIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010)
title_full SIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010)
title_fullStr SIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010)
title_full_unstemmed SIMULATION OF VOLCANIC ASH DISTRIBUTION WITH FALL3D (CASE STUDY : MOUNT MERAPI ERUPTION ON NOVEMBER 2010)
title_sort simulation of volcanic ash distribution with fall3d (case study : mount merapi eruption on november 2010)
url https://digilib.itb.ac.id/gdl/view/18581
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