Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USA

The West Branch of the Little River in Stowe, Lamoille County, Vermont has been widely studied, and this area is regularly subject to flooding. The West Branch joins the Little River, which flows into the Winooski and drains into Lake Champlain. This area has undergone extensive development as an ec...

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Main Authors: Florence Elfriede S. Silalahi, Fahrul Hidayat
Format: Article
Language:English
Published: Diponegoro University 2020-04-01
Series:Geoplanning: Journal of Geomatics and Planning
Subjects:
Online Access:https://ejournal.undip.ac.id/index.php/geoplanning/article/view/24177
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spelling doaj-cf24cb9bfca54e81852c934e4b22f4952021-03-12T09:12:36ZengDiponegoro UniversityGeoplanning: Journal of Geomatics and Planning2355-65442020-04-0162899810.14710/geoplanning.6.2.89-9816377Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USAFlorence Elfriede S. Silalahi0Fahrul Hidayat1Western Michigan University, Geological and Environmental Sciences, USA; Geospatial Information AgencyGeospatial Information AgencyThe West Branch of the Little River in Stowe, Lamoille County, Vermont has been widely studied, and this area is regularly subject to flooding. The West Branch joins the Little River, which flows into the Winooski and drains into Lake Champlain. This area has undergone extensive development as an economic response to the ski resort industry over the past 50 years, and the recreational pathway is on the banks of the river. The Little River is adjusting to the loss of historic floodplain area, channel modifications (straightening and gravel mining), and runoff changes. In this project, a DEM with 10 and 30 meters resolution will be used to determine the watershed area for the outlet point at the south of Stowe for hydrological analysis. This project intends to describe the watershed flow direction with a unit hydrograph that shows when water discharge at the outlet is at its height during a rainfall event and produce the floods prediction map by predicting the nature of flood events to help in planning and responding to flood events effectively using ArcGIS Pro 2.0. The results show the time it takes water to flow to the outlet ranges from 0 seconds (rain that falls on the outlet itself) to over 8 hours and 46 minutes. The amount of water has accumulated, indicating that water will flow at its fastest when funneling toward the outlet point downstream of the town with no exception, indicating that water will flow at its fastest when funneling toward the outlet point downstream of the town.https://ejournal.undip.ac.id/index.php/geoplanning/article/view/24177little river, flood, unit hydrograph, geographic information systems (gis), arcgis pro
collection DOAJ
language English
format Article
sources DOAJ
author Florence Elfriede S. Silalahi
Fahrul Hidayat
spellingShingle Florence Elfriede S. Silalahi
Fahrul Hidayat
Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USA
Geoplanning: Journal of Geomatics and Planning
little river, flood, unit hydrograph, geographic information systems (gis), arcgis pro
author_facet Florence Elfriede S. Silalahi
Fahrul Hidayat
author_sort Florence Elfriede S. Silalahi
title Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USA
title_short Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USA
title_full Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USA
title_fullStr Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USA
title_full_unstemmed Modelbuilder and Unit Hydrograph for Flood Prediction and Watershed Flow Direction Determination at The West Branch of The Little River, Stowe, Lamoille County, Vermont, USA
title_sort modelbuilder and unit hydrograph for flood prediction and watershed flow direction determination at the west branch of the little river, stowe, lamoille county, vermont, usa
publisher Diponegoro University
series Geoplanning: Journal of Geomatics and Planning
issn 2355-6544
publishDate 2020-04-01
description The West Branch of the Little River in Stowe, Lamoille County, Vermont has been widely studied, and this area is regularly subject to flooding. The West Branch joins the Little River, which flows into the Winooski and drains into Lake Champlain. This area has undergone extensive development as an economic response to the ski resort industry over the past 50 years, and the recreational pathway is on the banks of the river. The Little River is adjusting to the loss of historic floodplain area, channel modifications (straightening and gravel mining), and runoff changes. In this project, a DEM with 10 and 30 meters resolution will be used to determine the watershed area for the outlet point at the south of Stowe for hydrological analysis. This project intends to describe the watershed flow direction with a unit hydrograph that shows when water discharge at the outlet is at its height during a rainfall event and produce the floods prediction map by predicting the nature of flood events to help in planning and responding to flood events effectively using ArcGIS Pro 2.0. The results show the time it takes water to flow to the outlet ranges from 0 seconds (rain that falls on the outlet itself) to over 8 hours and 46 minutes. The amount of water has accumulated, indicating that water will flow at its fastest when funneling toward the outlet point downstream of the town with no exception, indicating that water will flow at its fastest when funneling toward the outlet point downstream of the town.
topic little river, flood, unit hydrograph, geographic information systems (gis), arcgis pro
url https://ejournal.undip.ac.id/index.php/geoplanning/article/view/24177
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