Types of Flooding
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Evaluating Snowmelt Runoff Generation in a Discontinuous Permafrost
Evaluating snowmelt runoff generation in a discontinuous Nordic Hydrology permafrost catchment using stable isotope, hydrochemical and hydrometric data* S.K. Carey1 and W.L. Quinton2 1Department of Geography and Environmental Studies, Carleton University, Ottawa, Ontario, Canada K1S 5B6 Vol 35 No 4 pp 309–324 E-mail: [email protected] 2Department of Geography, Simon Fraser University, Burnaby, British Columbia, Canada V5A 1S6 Received 1 November 2003; accepted in revised form 15 June 2004 Abstract Research on snowmelt runoff generation in discontinuous permafrost subarctic catchments has highlighted the role of: (i) permafrost in restricting deep percolation and sustaining near-surface water tables and (ii) the surface organic layer in rapidly conveying water to the stream. Conceptual models of runoff generation have largely been derived from hydrometric data, with isotope and hydrochemical data having only limited q application in delineating sources and pathways of water. In a small subarctic alpine catchment within the Wolf IWA Publishing 2004 Creek Research Basin, Yukon, Canada, snowmelt runoff generation processes were studied during 2002 using a mixed methods approach. Snowmelt timing varied between basin slopes, with south-facing exposures melting prior to permafrost-underlain north-facing slopes. The streamflow freshet period begain after 90% of snow had melted on the south-facing slope and coincided with the main melt period on the north-facing slope, indicating that contributing areas were largely defined by permafrost distribution. Stable isotope (d18O) and hydrochemical parameters (dissolved organic carbon, specific conductivity, pH) suggest that, at the beginning of the melt period, meltwater infiltrates soil pores and resides in temporary storage. As melt progresses and bare ground appears, thawing of soils and continued meltwater delivery to the slopes allows rapid drainage of this meltwater through surface organic layers. -
Provincial Freshet and Flood Status
Dashboard # Provincial Lead Contact: Media Relations contact: Provincial Freshet and Flood Status Manager, River Forecast Centre & Flood Safety Provincial Information Coordination Officer Date: June 24th, 2021, 4:00 pm Freshet 12 - George Roman Tyler Hooper 2021 Water Management Branch, Public Affairs Officer Ministry of Forests, Lands, Natural Resource [email protected] Operations and Rural Development (FLNRORD) 250-213-8172 [email protected] 250-896-2725 Provincial Summary Several streams and rivers are flowing higher this week than seasonal due the unprecedented historic heat resulting in a number of Flood Warnings, Flood Watches and High Streamflow Advisories. In general, stream flows will begin to recede over the next week. The Fraser River is expected to rise into the weekend; however, flows are forecast to remain below their earlier 2021 peaks. Provincial staff, local government staff, First Nations, and other parties continue to monitor the situation and support the implementation of flood emergency preparedness, response, and recovery. The public is advised to stay clear of all fast-flowing rivers and streams and potentially unstable riverbanks during spring high streamflow periods. Weather (Current and Forecast) Temperatures have reduced from the historic heat we recently experienced. As the ridge that resulted in the high temperatures moves east there is increased risk of instability leading to thunder and lightening. Limited precipitation is expected over the next several days. Flood Warnings and Advisories River Conditions and Outlook Flood Warning The historic heat event has led to historic snow melt. Many streams responded to the extreme heat and high elevation snow and glacial • Upper Fraser River melt. -
Severe Weather Safety Guide Flash Flooding
What causes River Flooding? Stay informed! • Persistent storms over the same area for long Listen to NOAA Weather Radio, local radio or Severe periods of time. television for the latest weather and river forecasts. • Combined rainfall and snowmelt • Ice jams Weather • Releases from man made lakes • Excessive rain from tropical systems making Safety landfall. How does the NWS issue To check out the latest river forecast information Guide and current stages on our area rivers, visit: Flood/Flash Flood Warnings? http://weather.gov/pah/ahps Flash Check out the National Weather Service Paducah website for the latest information at Flooding weather.gov/paducah Call for the latest forecast from the National Weather Service’s Weather Information Now number: Paducah, KY: 270-744-6331 Evansville, IN: 812-425-5549 National Weather Service forecasters rely on a A reference guide from your network of almost 10,000 gages to monitor the National Oceanic & Atmospheric Administration height of rivers and streams across the Nation. National Weather Service National Weather Service This gage data is only one of many different 8250 Kentucky Highway 3520 Paducah, Kentucky sources for data. Forecasters use data from the Doppler Radar, surface weather observations, West Paducah, KY 42086 snow melt/cover information and many other 270-744-6440 different data sources in order to monitor the threat for flooding. FLOODS KILL MORE PEOPLE FACT: Almost half of all flash flood Flooding PER YEAR THAN ANY OTHER fatalities occur in vehicles. WEATHER PHENOMENAN. fatalities occur in vehicles. Safety • As little as 6 inches of water may cause you to lose What are Flash Floods ? control of your vehicle. -
New York State Canal Corporation Flood Warning and Optimization System
K19-10283720JGM New York State Canal Corporation Flood Warning and Optimization System SCOPE OF SERVICES K19-10283720JGM Contents 1 Background of the Project........................................................................................................... 3 2 Existing FWOS features ............................................................................................................... 5 2.1 Data Import Interfaces ............................................................................................................ 5 2.2 Numeric Models ...................................................................................................................... 5 2.2.1 Hydrologic Model............................................................................................................. 6 2.2.2 Hydraulic Model .............................................................................................................. 6 2.3 Data Dissemination Interfaces .................................................................................................. 6 3 Technical Landscape ................................................................................................................... 7 3.1 Software ................................................................................................................................. 7 3.1.1 Systems......................................................................................................................... 7 3.1.2 FWOS Software .............................................................................................................. -
2019 Freshet Update No. 1
MEDIA RELEASE FOR IMMEDIATE RELEASE March 8, 2021 2021 Freshet Update #1 BRACEBRIDGE, ON – Springtime is fast approaching and flooding in low lying areas of the Town is a potential risk due to melting snow and spring rainfall. With the freshet events of 2019 still very clear in our minds, the Town of Bracebridge wishes to remind its residents and visitors that freshet preparations should be undertaken by those in areas prone to flooding. The Town of Bracebridge is committed to the safety of our residents and visitors, as well as the protection of property. With this in mind, we wish to keep the public informed so that they can be prepared to lessen the effects of flooding events should they occur this year. Town of Bracebridge emergency planning officials are working closely with their counterparts from the District Municipality of Muskoka and the other municipalities in Muskoka to ensure a consistent flow of information to the public in the event of a flood occurrence. As we progress through the 2021 spring freshet, the Town will issue freshet updates to assist in flood protection and mitigation. These updates may include: Ministry of Natural Resources and Forestry (MNRF) flood bulletins, road closure locations, sandbag availability, safety tips or other relevant flood information. The following information, together with supplementary items found on the Town’s website and the links contained in this update, provide valuable suggestions to assist property owners in preparation for the 2021 spring freshet: Ministry of Natural Resources and Forestry (MNRF) As part of their ongoing responsibilities for the management of area watersheds, the MNRF: • Monitors water levels in major Muskoka lakes and rivers, and regulates dams as appropriate to runoff conditions. -
Population Dynamics of the Eastern Oyster in the Northern Gulf of Mexico Benjamin S
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School 2012 Population dynamics of the eastern oyster in the northern Gulf of Mexico Benjamin S. Eberline Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Environmental Sciences Commons Recommended Citation Eberline, Benjamin S., "Population dynamics of the eastern oyster in the northern Gulf of Mexico" (2012). LSU Master's Theses. 567. https://digitalcommons.lsu.edu/gradschool_theses/567 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. POPULATION DYNAMICS OF THE EASTERN OYSTER IN THE NORTHERN GULF OF MEXICO A Thesis Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Master of Science in The School of Natural Resources by Benjamin S. Eberline B.S., Virginia Polytechnic Institute and State University, 2009 May 2012 Acknowledgements I would like to thank the Louisiana Sea Grant College Program for funding this project. I would also like to thank all those who took extra time and willingly gave their expertise in order to further this project: Patrick Banks, Keith Ibos, Brian Lezina, and Gary Vitrano from Louisiana Department of Wildlife and Fisheries; Lane Simmons and Dave Walters from United States Geological Survey; and Dr. -
Canal and River Bank Stabilisation for Protection Against Flash Flood and Sea Water Intrusion in Central Vietnam
CANAL AND RIVER BANK STABILISATION FOR PROTECTION AGAINST FLASH FLOOD AND SEA WATER INTRUSION IN CENTRAL VIETNAM V. Thuy1, I. Sobey2 and P. Truong3 1 Department of Agriculture and Rural Development, Quang Ngai, Vietnam 2Kellog Brown Roots, Quang Ngai Natural Disaster Mitigation Project [email protected] 3 TVN Director and East Asia and South Pacific Representative, 23 Kimba St, Chapel Hill, Brisbane 4069, Australia [email protected] Abstract Quang Ngai, a coastal province in central Vietnam, is prone to flash flood caused by high annual rainfall, with 70% (2300mm/yr) falling over three months and steep terrain resulting in high velocity water flows. This often leads to flash floods in mountainous areas and large scale flooding in low-lying areas. The high velocity flows and flooding cause severe erosion on dike, canal and river banks built to protect farm land from flooding in the rain season and sea water intrusion in the dry season. Therefore the stability of these measures provides the local community a protection against flash flood and sea water intrusion at the same time. Both vegetative measures and hard structures such as rock and concrete have been used in the past to protect these banks, but they are ineffective partly due to the local sandy soils used to build them and partly to the strong current. Although vetiver grass has been used very successfully for flood erosion control in the Mekong Delta of southern Vietnam, where flow velocity is relatively slow, it has not been used under very strong current. As a last resort, vetiver grass was tested for its effectiveness in protecting the banks of these rivers and canals. -
River Valley Civilizations
FCPS World I SOL Standards: WHI 3a, 3b and 3e River Valley Civilizations: China (2000 B.C.E.-200 B.C.E.) You Mean Yellow Soil Helped Ancient China? Geography of the Huang He Many geographic features like the Yellow Sea, East China Sea and the Pacific Oceanisolated Ancient China from other civilizations. Ancient China’s first civilizations formed near the Huang He, also known as the Yellow River. Just like other river valley civilizations, the Huang He would flood and leave behind large amounts of yellowish fertile soil called loess. The flooding of the Yellow River was both a good and bad thing for the Chinese. The fertile soil would help farmers with their crops but it would also bring terrible floods killing people and destroying homes. This is why it was also called “China’s sorrow.” Although China was protected by rivers, oceans and mountains, the geography did not completely protect the people. Ancient China had many invasions from the west and the north throughout their history. China River Valley Civilization: Huang He Valley Source: http://www.marshallcavendishdigital.com/articledisplayresult/17/4631/47381 Ancient Chinese Culture The family was the most important part of ancient Chinese society. The father controlled the household and made the important decisions. There was a great emphasis on respect for elders, and children were expected to honor their mother and father. The Chinese also believed in the worship of their ancestors. The spirits of these dead family members would bring either good fortune or disaster. The Chinese had a polytheistic religion. Priests would talk to these gods through the use of oracle bones. -
Flood-Inundation Maps for the Meramec River at Valley Park and at Fenton, Missouri, 2017
Prepared in cooperation with the U.S. Army Corps of Engineers, St. Louis Metropolitan Sewer District, Missouri Department of Transportation, Missouri American Water, and Federal Emergency Management Agency Region 7 Flood-Inundation Maps for the Meramec River at Valley Park and at Fenton, Missouri, 2017 Scientific Investigations Report 2017–5116 U.S. Department of the Interior U.S. Geological Survey Cover. Flooding from the Meramec River in Valley Park, Missouri. Upper left photograph taken December 30, 2015, by David Carson, St. Louis Post-Dispatch, used with permission. Lower right photograph taken December 31, 2015, by J.B. Forbes, St. Louis Post-Dispatch, used with permission. Back cover. Flooding from the Meramec River near Eureka, Missouri, December 30, 2015. Photographs by David Carson, St. Louis Post-Dispatch, used with permission. Flood-Inundation Maps for the Meramec River at Valley Park and at Fenton, Missouri, 2017 By Benjamin J. Dietsch and Jacob N. Sappington Prepared in cooperation with the U.S. Army Corps of Engineers, St. Louis Metropolitan Sewer District, Missouri Department of Transportation, Missouri American Water, and Federal Emergency Management Agency Region 7 Scientific Investigations Report 2017–5116 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Acting Director U.S. Geological Survey, Reston, Virginia: 2017 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. -
Q. What Is a Freshet? A
Q. What is a freshet? A. A sudden rise in the level of a stream, or a flood, caused by heavy rains or the rapid melting of snow and ice between May and mid-July. Q. Is there going to be a big flood this year? A. Much depends on the weather, and snowpack both of which are difficult to predict. Q. What is the chance of a major flood? A. It is impossible to know in advance how high water levels will rise. The severity of flooding, and whether or not significant flooding occurs on major river systems, will depend primarily on the weather. Q. When will the flood hit? A. There is no way of knowing when water levels will peak. But river levels will not rise suddenly. We will have warning of high water flows several days in advance. We will continue to monitor water levels constantly and keep the public informed through the media. Q. What does the City do to prepare for an annual freshet? A. In recent years, the City has completed a number of diking system upgrades to prepare for Fraser River freshets. In addition to large capital projects, the City also completes numerous maintenance activities throughout the year to ensure the diking system is maintained. Q. How much notice will a person have that their area is going to flood? A. Weather patterns and forecasts will be the primary indicator of Fraser River water levels, and the City relies heavily on the Ministry of Environment River Forecast Center for regularly updated flood forecasts. -
Frequently Asked Questions About a Stormwater Utility
Frequently asked questions about a Stormwater Utility and Stormwater in general: What will the Stormwater Utility do? The O’Fallon Stormwater Utility will fix drainage problems if the water is coming from a public source, such as a street or drainage system, and if the repair serves some public good. (See Wills and Won’ts for additional detail on what the Stormwater Utility will do.) Qualifying problems include: • Flooding of a living space • Severe stream bank erosion • Blocked creeks, storm drainage pipes or drainage ditches • Undersized storm drainage pipes or culverts • Sinkholes over storm drainage pipes Problems that do not qualify include: • Yard flooding • Drainage problems caused by landscaping • Drainage concerns caused by roofing or gutter problems • Water that flows from adjoining property • Wet areas due to underground springs or wetlands • Water standing in a drainage ditch on private property that is not in a drainage easement Why is there a Storm Water fee? The O’Fallon Stormwater will fee pay for local efforts to reduce flooding and reduce water pollution. Stormwater is rain water that does not soak into the ground. It flows into our storm drainage system without being treated or cleaned. Managing stormwater runoff is crucial to O’Fallon’s quality of life. That includes maintaining and improving our stormwater drainage system to reduce flood risks and working to reduce pollution levels in our creeks and lakes. The cost of O’Fallon's stormwater program is anticipated to be funded by the fee, Prop S and General funds. The fee is based on: 1. how much each property contributes to stormwater runoff, and 2. -
2019 Spring Flood – Questions and Answers
Ottawa River Regulation Planning Board www.ottawariver.ca Ottawa River Commission de planification Regulation de la régularisation Planning Board de la rivière des Outaouais 2019 Spring Flood – Questions and Answers Message from the Ottawa River Regulation Planning Board The 2019 spring flood has been challenging and difficult to say the least, affecting thousands of people’s lives. Many concerned citizens have reached out to us since the start of the spring flood to share their experience and seek answers to their questions. Many people enquired about the causes of the spring flood, trying to have a better understanding of the regulation of flows in the Ottawa River Basin and what means, if any, could be used to further alleviate the flood impacts. In order to respond to these enquiries, we are happy to be releasing today a series of questions and answers that will address some of the most often asked questions during the spring flood of 2019. We consider these answers to be ‘preliminary’ as the member agencies will require time to conduct the post spring flood analyses. In the months to come, we will be reviewing conditions of the spring flood and will be preparing a summary document about the 2019 spring flood conditions, similar to the document1 we had prepared following the 2017 flood. In Ontario and Quebec, governments at all levels, federal, provincial, and municipal levels, take part in the protection of the residents against flooding. Our part, which deals with management of the flow from the principal reservoirs, can sometimes be difficult to explain. We have done our best to explain it in plain words in this document and hope that you will find it informative.