The search results explanations of hydrological data
|
|
- Pamela Dennis
- 5 years ago
- Views:
Transcription
1 Introduction The search results explanations of hydrological data Depending on the parameter, the instrumental measuring or visual observation method is used for the hydrological observations. Instrumentally measured results are recorded in a digital format with respective units, but the visual results of the observations are recorded in coded form. Information from data search results are described with codes for these visually observed hydrological parameters: Water object situation; characterization of ice conditions and location; amount of ice; ice width; ice closeness; form of ice; ice development stage. Water object situation Information about water object situation in both winter and summer is described in coded form from hydrological gauge stations, which are located in rivers, lakes and reservoirs. is five-figure combination: Characterization of water object situation Intensity of the phenomenon The first three figures characterize water object situation. Transcript with codes see the table below. The last two figures characterize intensity of phenomenon in water object. To encode intensity of phenomena use numbers: 01, 02, 03, 04, 05, 06, 07, 08, 09, 10, which indicate, that observed phenomenon covers respectively 10, 20, 30, 40, 50, 60, 70, 80, 90, un 100% from river width or body of visible water area. If the intensity does not determine, than use 00. The characteristic term of water object situation Ice development and destruction 511 grease ice 512 slush (thin) 512 slush (moderate or thick) 513 border ice in lakes and reservoirs (width less than 100 m) 514 fast ice in lakes and reservoirs (width more than 100 m) 515 shore ice 516 thin ice flow; ice drift in lakes and reservoirs 516 moderate or thick ice flow; ice drift in lakes and reservoirs 517 ice flow; ice from tributary, lake, reservoir 518 ice flow over ice cover 519 thin slush ice run 519 moderate or thick slush ice run 520 anchor ice 521 anchor iceland 522 immersed ice (on coastal shelf after level drop) 523 ice piles on the river bank 524 ice closing dike in the gauge cross-sections LEGMC The searching results explanations of hydrological data 1
2 The characteristic term of water object situation 525 ice closing dike upstream the gauge 526 ice closing dike downstream the gauge 527 channel is narrowed by ice formations downstream the gauge (connected with water level increase) 528 channel is narrowed by ice formations upstream the gauge (connected with water level drop) 530 ice jam upstream the gauge 531 ice jam downstream the gauge 532 ice jam is destroyed artificially 534 slush jam upstream the gauge 535 slush jam downstream the gauge 536 slush jam is destroyed artificially 537 water on ice 538 water flows over the ice surface (river frozen through; when water is under ice) 539 opening water near the river bank 540 ice has darkened 541 puddle 542 ice has lifted 543 initial ice movement 544 open channel (in ice) ice lane 545 ice melts on a place 546 ice ledge 547 glimmer ice 548 loose pack ice in lakes, reservoirs and rivers mouth stages 549 pancake ice in lakes, reservoirs and rivers mouth stages 550 ice field in lakes, reservoirs; river mouth stage field ice 551 crushed ice in lakes, reservoirs and rivers mouth stages 552 ground hummock 553 ice carries (carried away) from the coast - lakes, reservoirs 554 stranded pressure ice - lakes, reservoirs Ice cover 563 incompleted ice cover 564 opening in ice cover 565 ice over 566 hummocked ice cover 567 hummocked ice ridge 568 slush ice path 569 slush under ice 570 cracks in ice 571 flooding ice 572 ice bridge 573 layered ice (ice cover consists from different layers, between them is situated water or air intermediate layer) 574 depth ice (in consequence of immersed ice or river frozen through) 575 river (lake) frozen through 576 ice artificially destroyed (with icebreaker, dynamite and other technical features) 577 water on river ice Additional details information group for water object situation 600 Open water (chanell) 664 slack water (cross arm, which is located upstream or downstream, is frozen through or dried up) 660 wadi - river has dried up Overgrowing LEGMC The searching results explanations of hydrological data 2
3 The characteristic term of water object situation 622 aquatic vegetation at river bank 623 aquatic vegetation in whole cross - section 626 aquatic vegetation in gauge cross-section mown-out 627 aquatic vegetation laid down on river bed (in autumn) 628 aquatic vegetation has silted up (when fish pounds are lowered et.) 629 aquatic vegetation was lost because of river pollution Characterization of ice conditions and location Information about characterization of ice conditions and location is described in the coded form with two marks in coastal hydrological the gauges. The characteristic term of ice conditions and location Ice basic phenomena 00 early ice appearance (no old ice) 01 early ice appearance (old ice is remained) 02 shore ice has formed 03 fast ice has formed (width more than 200) 04 young ice appearance from another area (drifted) 05 old ice appearance from another area (drifted) 06 repeated ice formation in observed gauge area 07 the sea is covered with static ice until visible horizon (total freezing) 08 repeated total freezing 09 the first ice shearing 10 fast ice is partly broken open 11 fast ice is absolutely broken open 12 the sea is completely purified from ice Pack ice characteristic peculiarities 13 ice concentration is increased 14 ice concentration is decreased 15 stranded pressure ice at the coast 16 strong ice compacting and hummocking 17 slush jam at the coast with ridges and ice fronts from hummocks 18 ice carries (carried away) from the coast 19 polynia Packing ice location 20 packing ice is evenly located over the entire surface of the sea 21 packing ice is predominantly located on the north side 22 packing ice is predominantly located on the east side 23 packing ice is predominantly located on the south side 24 packing ice is predominantly located on the west side 25 packing ice is predominantly located at the coast, ice is rare in the sea or the sea is ice free 26 packing ice is predominantly located far from the coast, ice is rare at the coast or open water 27 packing ice is predominantly located by separate fields 28 packing ice is predominantly located on zones 29 separate pieces of ice on the sea surface Amount of open water in balls; fields, where are no ice 30 no open water 31 amount of open water 1-2 ball 32 amount of open water 3 ball 33 amount of open water 4 ball 34 amount of open water 5 ball 35 amount of open water 6 ball LEGMC The searching results explanations of hydrological data 3
4 The characteristic term of ice conditions and location 36 amount of open water 7 ball 37 amount of open water 8 ball 38 amount of open water 9 ball 39 amount of open water 10 ball (ice free) Direction, where is observed open water 40 no open water 41 open water is observed on the NE 42 open water is observed on the E 43 open water is observed on the SE 44 open water is observed on the S 45 open water is observed on the SW 46 open water is observed on the W 47 open water is observed on the NW 48 open water is observed on the N 49 open water fields are observed in different directions Packing ice direction 50 ice does not move 51 ice is moving on the SW 52 ice is moving on the W 53 ice is moving on the NW 54 ice is moving on the N 55 ice is moving on the NE 56 ice is moving on the E 57 ice is moving on the SE 58 ice is moving on the S 59 packing ice direction cannot be determined 65 hummocking 1 ball 66 hummocking 2 ball 67 hummocking 3 ball 68 hummocking 4 ball 69 hummocking 5 ball 70 ice destruction 1 ball 71 ice destruction 2 ball 72 ice destruction 3 ball 73 ice destruction 4 ball 74 ice destruction 5 ball 80 no snow on the ice 81 height until 4 cm 82 height 5-9 cm 83 height cm 84 height cm 85 height cm 86 height cm 87 height cm 88 height cm 89 height 70 cm and more 98 Hummock ridge 99 Hummock front Ice hummocking in balls Ice destruction in balls Snow thickness on ice Separate ice forms LEGMC The searching results explanations of hydrological data 4
5 Amount of ice Information about amount of ice (both static and drifting) is given in balls from the coastal hydrological gauges. Ball indicates the part of aquatory, what is covered with ice. Amount of ice 1, 2, 3, 4, 5, 6, 7, 8, 9 or 10 balls indicate, that with ice is covered respectively 10, 20, 30, 40, 50, 60, 70, 80, 90 or 100 % from the sea aquatory. Amount of ice, ball Amount of ice, ball Ice width 0 ice free or less than 1 ball Information from the coastal hydrological gauges about ice width is determined in kilometres. It is coded by scale. Ice width, km Ice width, km 0 ice free less than until visible horizon and opposite bank, if it is farther than 15.0 km Ice concentration In the coastal hydrological gauges ice concentration is called as pieces of ice, included new ice forms, relative to area, where those are located, and it is expressed in balls. Ice concentration is observed by scale from 0 until 10 balls. Ice concentration graphic scale in balls Form of ice In the coastal hydrological gauges forms of ice are ice fields and those forms. Those are coded by scale. Form of ice 0 ice free 1 new ice (frazil ice, grease ice and slush ice, shuga, pancake ice) 2 brash ice LEGMC The searching results explanations of hydrological data 5
6 3 small ice cake (< 2 m across) 4 ice cake (2-20 m across) 5 small floe ( m across) 6 small floe ( m across) and ice cake (2-20 m across) 7 medium floe ( m across) 8 big floe ( m across) 9 vast floe (>2000m across) Ice stage of development Information from the coastal hydrological gauges about ice stage of development (age composition) are coded by scale. Ice stage of development 0 ice free 1 frazil ice, grease ice, slush ice, shuga 2 pancake ice 3 dark nilas (<5 cm thick) 4 light nilas (5-10 cm thick) 5 grey ice (10-5cm thick) 6 grey-white ice (15-30cm thick) 7 thin-first-year ice/ white ice, first stage (30-50cm thick) 8 thin-first-year ice/ white ice, second stage (50-70 cm thick) 9 medium first-year ice ( cm thick) LEGMC The searching results explanations of hydrological data 6
The ice season
The ice season 2007-2008 Author: Jouni Vainio 1 Co-authors: Patrick Eriksson 1, Natalija Schmelzer 2, Anette Jönsson 3, Giedrius Ezerskis 4, Polina Soloshchuk 5, Natalia Fedorenko 5 and Yuriy Shiskin 6
More informationThe ice season
The ice season 2005-2006 Author: Jouni Vainio 1 Co-authors: Simo Kalliosaari 1, Natalija Schmelzer 2, Torbjörn Grafström 3, Inga Dailidiene 4, Evgeni Komissarov 5 and P. Soloshchuk 5 Key Message The ice
More informationThe Ice Season
The Ice Season 2006-2007 Author: Jouni Vainio 1 Co-authors: Simo Kalliosaari 1, Natalija Schmelzer 2, Torbjörn Grafström 3, Giedrius Ezerskis 4, Evgeni Komissarov 5, P. Soloshchuk 5, N. Fedorenko 5 and
More informationglacier Little Ice Age continental glacier valley glacier ice cap glaciation firn glacial ice plastic flow basal slip Chapter 14
Little Ice Age glacier valley glacier continental glacier ice cap glaciation firn glacial ice plastic flow basal slip glacial budget zone of accumulation zone of wastage glacial surge abrasion glacial
More informationIntroduction to Safety on Glaciers in Svalbard
Introduction to Safety on Glaciers in Svalbard Content Basic info on Svalbard glaciers Risk aspects when travelling on glaciers Safe travel on glaciers UNIS safety & rescue equipment Companion rescue in
More informationPresentation Overview
DON NARROWS Historical and Existing Conditions March 29, 2008 Presentation Overview 1. Project Location and Background 2. Historical Context How did the Don Narrows Come to Be? 3. The Today 4. Next Steps
More informationPHYSICAL GEOGRAPHY GEOGRAPHY EARTH SYSTEMS COASTAL SYSTEMS FLUVIAL SYSTEMS
PHYSICAL GEOGRAPHY EARTH SYSTEMS FLUVIAL SYSTEMS COASTAL SYSTEMS PHYSICAL GEOGRAPHY CORRIES / CIRQUES A Corrie or Cirque is the armchair shaped hollow that was the birthplace of a glacier. It has steep,
More informationDIDYMO SURVEY, LOWER FRYINGPAN RIVER, BASALT, COLORADO 2015
DIDYMO SURVEY, LOWER FRYINGPAN RIVER, BASALT, COLORADO 2015 Second Annual Report PREPARED FOR: ROARING FORK CONSERVANCY PREPARED BY: COLORADO MOUNTAIN COLLEGE NATURAL RESOURCE MANAGEMENT PROGRAM TIMBERLINE
More informationGLACIER STUDIES OF THE McCALL GLACIER, ALASKA
GLACIER STUDIES OF THE McCALL GLACIER, ALASKA T John E. Sater* HE McCall Glacier is a long thin body of ice shaped roughly like a crescent. Its overall length is approximately 8 km. and its average width
More informationChapter 14. Glaciers and Glaciation
Chapter 14 Glaciers and Glaciation Introduction Pleistocene Glaciations: A series of "ice ages" and warmer intervals that occurred 2.6 million to 10,000 years ago. The Little Ice Age was a time of colder
More informationUnit 1: Physical Environment Glaciated Landscapes
Unit 1: Physical Environment Glaciated Landscapes Corries Corries are bowl-shaped hollows high up in the mountains. They are formed in the following way: Snow collects in a hollow on a mountainside (usually
More informationGlaciology. Water. Glacier. Moraine. Types of glacier-dammed lakes. Mechanics of jökulhlaup
A Jökulhlaup Jökulhlaup. Catastrophic events where large amounts of water are suddenly discharged. Jökulhlaup s are a sudden and rapid draining of a glacier dammed lake or of water impounded within a glacier.
More informationThe Potentially Dangerous Glacial Lakes
Chapter 11 The Potentially Dangerous Glacial Lakes On the basis of actively retreating glaciers and other criteria, the potentially dangerous glacial lakes were identified using the spatial and attribute
More informationTypical avalanche problems
Typical avalanche problems The European Avalanche Warning Services (EAWS) describes five typical avalanche problems or situations as they occur in avalanche terrain. The Utah Avalanche Center (UAC) has
More informationE-9093 Ice Class Ship Structures
E-9093 Ice Class Ship Structures by Claude Daley Professor of Ocean and Naval Architectural Engineering Part 1 Overview of Arctic Shipping Topics Ice Class Ships 1 Overview of Arctic Shipping Ice What
More informationZoran Đuroković, B. Sc. (Civ.Eng.) Davor Haničar, B. Sc. (Civ.Eng.) Ladislav Grđan, B. Sc. (Civ.Eng.) Silvio Brezak, B. Sc. (Civ.Eng.
FLOOD PROTECTION EXPERIENCES ON THE DRAVA RIVER BASIN IN CROATIA Maribor, September 23-25 2008 Zoran Đuroković, B. Sc. (Civ.Eng.) Davor Haničar, B. Sc. (Civ.Eng.) Ladislav Grđan, B. Sc. (Civ.Eng.) Silvio
More informationComparison Pictures of Receding Glaciers
Comparison Pictures of Receding Glaciers In the photo above, the west shoreline of Muir Inlet in Alaska's Glacier Bay National Park & Preserve is shown as it appeared in 1895. Notice the lack of vegetation
More information1 Glacial Erosion and
www.ck12.org Chapter 1. Glacial Erosion and Deposition CHAPTER 1 Glacial Erosion and Deposition Lesson Objectives Discuss the different erosional features formed by alpine glaciers. Describe the processes
More informationMount Rainier National Park November 2006 Flood Damage
On November 6 and 7, 2006, Mount Rainier National Park received 18 inches of rain in 36 hours. This presentation summarizes the extensive flood damage that occurred throughout the park. Updated November
More informationREADING QUESTIONS: Chapter 7, Glaciers GEOL 131 Fall pts. a. Alpine Ice from larger ice masses flowing through a valley to the ocean
READING QUESTIONS: Chapter 7, Glaciers GEOL 131 Fall 2018 63 pts NAME DUE: Tuesday, October 23 Glaciers: A Part of Two Basic Cycles (p. 192-195) 1. Match each type of glacier to its description: (2 pts)
More informationObserving Subtleties: Traditional Knowledge and Optimal Water Management of Lake St. Martin
Observing Subtleties: Traditional Knowledge and Optimal Water Management of Lake St. Martin Myrle Traverse and Richard Baydack Abstract Lake St. Martin First Nation is an Anishinaabe community situated
More information2014 floods in Serbia
16 th Meeting of WGF, Rim, 9-10 October 2014 2014 floods in Serbia Radovanka Pavlović Ministry of Agriculture and Environmental Protection Republic Water Direcrorate, Belgrade, Serbia Specific cyclone
More informationAPPENDIX D: SUSTAINABLE TRAIL DESIGN. APPENDICES Town of Chili Parks and Recreation Master Plan Update
APPENDIX D: SUSTAINABLE TRAIL DESIGN APPENDICES Town of Chili Parks and Recreation Master Plan Update Sustainable Trail Construction Sustainable trails are defined by the US Forest Service as trails having
More informationGEOSPATIAL ANALYSIS OF GLACIAL HAZARDS PRONE AREAS OF SHIGAR AND SHAYOK BASINS OF PAKISTAN. By Syed Naseem Abbas Gilany
GEOSPATIAL ANALYSIS OF GLACIAL HAZARDS PRONE AREAS OF SHIGAR AND SHAYOK BASINS OF PAKISTAN By Syed Naseem Abbas Gilany PRESENTATION OUTLINE Introduction Problem Statement / Rationale Objectives Material
More information5 MAP SPECIFICATION FOR SKI-ORIENTEERING
5 MAP SPECIFICATION FOR SKI-ORIENTEERING 5.1 General Maps for ski orienteering are based on the specifications for foot-orienteering maps. However in order to meet the specific requirements put on the
More informationHISTORICAL FLOOD LEVELS
5.36 5.02 3.58 3.59 3.68 3.67 3.21 2.87 3.01 2.91 2.8 3.78 2.42 4.02 2.4 2.37 2.35 2.06 2.41 2.39 2.39 2.37 2.39 2.4 2.39 2.14 2.06 2.39 2.41 2.42 2.31 2.14 2.3 1.5 2.38 2.16 2.43 1.5 2.43 1.91 4.93 4.63
More informationDRAINAGE BASINS OF THE SEA OF OKHOTSK AND SEA OF JAPAN
60 DRAINAGE BASINS OF THE SEA OF OKHOTSK AND SEA OF JAPAN SEA OF OKHOTSK AND SEA OF JAPAN 61 62 AMUR RIVER BASIN 66 LAKE XINGKAI/KHANKA 66 TUMEN RIVER BASIN 62 SEA OF OKHOTSK AND SEA OF JAPAN This chapter
More informationGlaciers and Glaciation Earth - Chapter 18 Stan Hatfield Southwestern Illinois College
Glaciers and Glaciation Earth - Chapter 18 Stan Hatfield Southwestern Illinois College Glaciers Glaciers are parts of two basic cycles: 1. Hydrologic cycle 2. Rock cycle A glacier is a thick mass of ice
More informationCoastal Impact on barrier Islands: Application to Praia de Faro
Coastal Impact on barrier Islands: Application to Praia de Faro Theocharis Plomaritis, Oscar Ferreira and Susana Costas RISCKIT Final Meeting This project has received funding from the European Union s
More information1.4 Understand how moving ice acts as an agent of erosion and deposition. (Chap. 2)
1.4 Understand how moving ice acts as an agent of erosion and deposition. (Chap. 2) There are two types of glaciation. Alpine Glaciation Continental Glaciation Distinguish between the terms alpine glaciation
More informationII. THE BOULDER CREEK DRAINAGE BASIN
II. THE BOULDER CREEK DRAINAGE BASIN This section provides an overview of the watersheds and flood hazards associated with Boulder Creek and South Boulder Creek including descriptions of the drainage basins,
More informationLeptis Magna. 9 LEPTIS MAGNA s NORTH COAST
9 LEPTIS MAGNA s NORTH COAST The following observations were made on August 24, 25 and 26, 2000, thanks to the kind hospitality of the late Professor André Laronde during his year 2000 campaign of the
More informationActual Climatic Conditions in ERB. Online Resource 1 corresponding to:
Actual Climatic Conditions in ERB. Online Resource 1 corresponding to: Article Title: Climatic Trends and Impact of Climate Change on Agriculture in an Arid Andean Valley. Journal Name: CLIMATIC CHANGE
More informationSpecification for Grip blocking using Peat Dams
Technical Guidance Note 1 Specification for Grip blocking using Peat Dams 1. Introduction Moorland drains (grips) have been dug across much of the Yorkshire upland peatlands. Many of these grips have become
More informationAPPENDIX A. Condition Survey of Pavements Concrete Mixture Proportions Used in Pavements Deicer Usage on Pavements Core Locations and Core Catalog
APPENDIX A (i) (ii) (iii) (iv) Condition Survey of Pavements Concrete Mixture Proportions Used in Pavements Deicer Usage on Pavements Core Locations and Core Catalog Report IPRF-01-G-002-05-7 Appendix
More informationLandscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age.
Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age. Key idea: Ice was a powerful force in shaping the landscape of the UK. In the past the climate has got colder
More informationGlaciers Earth 9th Edition Chapter 18 Mass wasting: summary in haiku form Glaciers Glaciers Glaciers Glaciers Formation of glacial ice
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Earth 9 th Edition Chapter 18 Mass wasting: summary in haiku form Ten thousand years thence big glaciers began to melt - called "global warming." are parts of two basic
More informationTwin Lakes Avalanche Incident 1/31/2016
Twin Lakes Avalanche Incident 1/31/2016 Location: Place State Published by: Dave Bingaman (PAC), George Halcom (PAC), and Kent May (PAC) Twin Lakes, Salmon River Mountains Idaho Date 01/31/2016 Time Summary
More information4/28/17. Clicker Question. Clicker Question. #37 Floods IV (Case Histories-Mississippi River Flood, 1993; Red River of North Flood, 1997)
GEOL 118 Final Exam Format similar to exams 1 and 2 Covers Lectures #27 40 (Global Climate Change I - Meteorite Impacts III) Web Exercise #6 - Due by 1 pm, Monday (5/1) 8:00 AM, Thursday, May 11 th Location
More informationThe Physical Geography of Long Island
The Physical Geography of Long Island A Bit About Long Island Length 118 miles Brooklyn to Montauk Geo202 Spring 2012 Width 23 miles at it s widest Area 1,400 square miles Formation of Long Island River
More informationTakeoff And Landing Performance Assessment TALPA. Chris Meyer MnDOT Aeronautics
Takeoff And Landing Performance Assessment TALPA Chris Meyer MnDOT Aeronautics TALPA Accident Case Study Runway Condition Assessment Matrix (RCAM) Resources for Education SWA Flight 1248, Chicago Midway,
More informationSnowmobile Safety Tips
Snowmobile Safety Tips The winter weather is bringing out snowmobilers, and safety officials are urging them to be careful. More than 200,000 registered snowmobiles hit Wisconsin s 25,000 miles of groomed
More informationRecrystallization of snow to form LARGE. called FIRN: like packed snowballs. the weight of overlying firn and snow.
Chapter 11 Glaciers BFRB P. 103-104, 104, 108, 117-120120 Process of Glacier Formation Snow does NOT melt in summer Recrystallization of snow to form LARGE crystals of ice (rough and granular) called
More informationAVALANCHE TERRAIN. Bill Glude Alaska Avalanche Specialists All photos and graphics Bill Glude unless otherwise noted.
Bill Glude Alaska Avalanche Specialists 20111202 All photos and graphics Bill Glude unless otherwise noted. AVALANCHE TERRAIN The Key Questions 1.) Could the terrain produce an avalanche?! a.) Where you
More informationInfluence of Amur River discharge on hydrological conditions of the Amurskiy Liman and Sakhalin Bay of the Sea of Okhotsk during a spring summer flood
Influence of Amur River discharge on hydrological conditions of the Amurskiy Liman and Sakhalin Bay of the Sea of Okhotsk during a spring summer flood Anastasiya Abrosimova, Igor Zhabin and Vyacheslav
More informationPermeable RECREATIONAL TRAILS
SMART EARTH SOLUTIONS Permeable RECREATIONAL TRAILS GEOWEB GEOPAVE GEOTERRA Innovative Solutions for Designing & Building Trails. Trail Surface Stabilization The key to planning and building trails into
More informationCity of Berkeley, CA Streetlight Condition Assessment
City of Berkeley, CA Streetlight Condition Assessment Project Background The City of Berkeley contracted with Tanko Lighting to evaluate the condition of the City s metal streetlights and develop a plan
More informationRM 2125 Troubleshooting Guide
Problems, possible causes and corrective action Problem Cause Corrective Action 1) Thick and Thin Sections. a) Partial Sections b) Shorter Sections in ribbon c) Section thickness varies from one section
More informationFormation of a Corrie
Formation of a Corrie A corrie looks rather like a armchair has been cut out of the rock face When a hill has been heavily eroded with 3 or 4 corries the jagged hill that is left is known as a pyramidal
More informationExtraordinary summer flood in a karst area: case study in Croatia
The Extremes ofthe Extremes: Exlraordinan' Floods (Proceedings ol'a symposium held at Reykjavik. Iceland. July 2000). IAHS Publ. no. 271. 2002. 133 Extraordinary summer flood in a karst area: case study
More informationGoing-to-the-Sun Road, Glacier National Park, MT, USA Avalanche Path Atlas
Going-to-the-Sun Road, Glacier National Park, MT, USA Avalanche Path Atlas Erich H. Peitzsch Daniel B. Fagre USGS Northern Rocky Mountain Science Center West Glacier, MT, USA Introduction... 2 Overview
More informationCARE, HANDLING & MAINTENANCE FOR ATTACK HOSE, LARGE DIAMETER HOSE (LDH), & SUPPLY HOSE
CARE, HANDLING & MAINTENANCE FOR ATTACK HOSE, LARGE DIAMETER HOSE (LDH), & SUPPLY HOSE North American Fire Hose Corporation is committed to providing the highest quality raw materials, unique design features,
More informationGOOSENECK SWAMP INFORMATION DAY - Saturday 14 th December 2013
GOOSENECK SWAMP INFORMATION DAY - Saturday 14 th December 2013 Progress of a restoration trial at Gooseneck Swamp - Grampians National Park, Victoria Gooseneck Swamp is situated at the far south-eastern
More informationGerman Meteorological Service. The quality of AMPS-Wind-Forecasts with regards to flight operations at Dronning Maud Land Season 2010/2011
The quality of AMPS-Wind-Forecasts with regards to flight operations at Dronning Maud Land Season 21/211 The quality of AMPS-Wind-Forecasts with regards to flight operations at Dronning Maud Land Season
More informationInstruction for edge trimming knife sharpening of M-Type shoe sewing machines
Instruction for edge trimming knife sharpening of M-Type shoe sewing machines 1. Introduction This instruction is a supplement to the instruction for use of electric table sharpener; thus the scope of
More informationHydrology Input for West Souris River IWMP
Hydrology Input for West Souris River IWMP Prepared by: Mark Lee Manitoba Water Stewardship 1 1 1 Overall view of: drainage area watershed characteristics gauging stations meteorological stations Runoff
More informationREADING QUESTIONS: Glaciers GEOL /WI 60 pts. a. Alpine Ice from larger ice masses flowing through a valley to the ocean
READING QUESTIONS: Glaciers GEOL 131 18/WI 60 pts NAME DUE: Tuesday, March 13 Glaciers: A Part of Two Basic Cycles (p. 192-195) 1. Match each type of glacier to its description: (2 pts) a. Alpine Ice from
More informationChapter 16 Glaciers and Glaciations
Chapter 16 Glaciers and Glaciations Name: Page 419-454 (2nd Ed.) ; Page 406-439 (1st Ed.) Part A: Anticipation Guide: Please read through these statements before reading and mark them as true or false.
More informationLesson 5: Ice in Action
Everest Education Expedition Curriculum Lesson 5: Ice in Action Created by Montana State University Extended University and Montana NSF EPSCoR http://www.montana.edu/everest Lesson Overview: Explore glaciers
More informationSYNOPSIS WEATHER AND SNOWPACK
Peak 6996 Avalanche Fatality Incident Report Glacier National Park, MT Date of Avalanche: 31 March 2010 Date of Investigation: 2 April 2010 Investigation Team: Erich Peitzsch (USGS), Ted Steiner (Chugach
More informationSAFETY AND ENVIRONMENTAL REGULATIONS OF THE POLAR CODE
SAFETY AND ENVIRONMENTAL REGULATIONS OF THE POLAR CODE Jorma Kämäräinen, Chief Adviser Regulation and Development Transport Operators and Technology Finnish Transport Safety Agency (Trafi) 10 th ARCTIC
More informationDATA BOOK IV : COST ESTIMATE
The Study on Comprehensive Disaster Prevention around Mayon Volcano DATA BOOK IV : COST ESTIMATE DT IV List of (1/5) Clearing and Grubbing ha 59,192.92 Excavation (Road way & Drainage) Mech. cu.m 80.55
More informationSingle and mass avalanching. Similarity of avalanching in space.
Single and mass avalanching. Similarity of avalanching in space. Pavel Chernous* Center for Avalanche Safety, "Apatit" JSC, Kirovsk, Russia ABSTRACT: Sometimes it is possible to observe only single avalanche
More informationNatural Factors Affecting the Level of Osoyoos Lake
Natural Factors Affecting the Level of Osoyoos Lake Background Osoyoos Lake is operated under conditions prescribed by the International Joint Commission (IJC) and Figure 1 shows the ranges within which
More informationAmerican Avalanche Association Forest Service National Avalanche Center Avalanche Incident Report: Long Form
American Avalanche Association Forest Service National Avalanche Center Avalanche Incident Report: Long Form Please send to: CAIC; 325 Broadway WS1; Boulder CO 80305; caic@qwest.net; Fax (303) 499-9618
More informationProgress Report March 2002 Project FIS Summary of Whitefish movement, Whitefish Lake Weir, Yukon Delta National Wildlife Refuge, Alaska, 2001
Progress Report March Project FIS 1-5 Summary of Whitefish movement, Whitefish Lake Weir, Yukon Delta National Wildlife Refuge, Alaska, 1 Frank G. Harris and Ken C. Harper U.S. Fish and Wildlife Service
More informationREPORT ON THE ICE EVENT 2017 IN THE DANUBE RIVER BASIN
REPORT ON THE ICE EVENT 2017 IN THE DANUBE RIVER BASIN www.icpdr.org REPORT ON THE ICE EVENT 2017 IN THE DANUBE RIVER BASIN 1 EDITORS Marina Babić Mladenović, Karoly Gombás, Igor Liška, László Balatonyi
More informationBudi Hadi Narendra Harris Herman Siringoringo Chairil Anwar Siregar. Research and Development Center for Forest
Budi Hadi Narendra Harris Herman Siringoringo Chairil Anwar Siregar Research and Development Center for Forest Background Coastal management should be wisely done as a part of watershed management. Typologically,
More informationHydrological study for the operation of Aposelemis reservoir Extended abstract
Hydrological study for the operation of Aposelemis Extended abstract Scope and contents of the study The scope of the study was the analytic and systematic approach of the Aposelemis operation, based on
More informationAvalanche Safety Guidelines This guideline is intended as a general introduction to this topic.
Introduction Worldwide, avalanches kill more than 150 people annually and thousands more are partly buried or injured. Although highway motorists and others can be involved in an avalanche, climbers, backcountry
More informationB.C. MINISTRY OF TRANSPORTATION. SA17 Local Area Specification #2 SMALL AIRPORT WINTER MAINTENANCE
1. OBJECTIVE B.C. MINISTRY OF TRANSPORTATION SA17 SMALL AIRPORT WINTER MAINTENANCE To ensure the Anahim Lake airport is kept open and safe for small airport users. 2. GENERAL PERFORMANCE SPECIFICATIONS
More informationAvalanche Accident Report
Hatcher Pass Avalanche Center POB 1223 Chickaloon, AK 99674 907-746-4566 info@hatcherpassavalanchecenter.org Avalanche Accident Report January 2, 2016 Avalanche Accident in Grubstake Gulch, Talkeetna Mountains,
More informationMOSE PROJECT: STATE-OF-THE-ART AND FUTURE DEVELOPMENT
AIPCN-France Third Mediterranean Days of Coastal and Harbour Engineering Troisièmes journées méditerranéennes de génie côtier et portuaire 23/05/2013 Marseille MOSE PROJECT: STATE-OF-THE-ART AND FUTURE
More informationSeismic Microzonation in Hurghada City (EGYPT)
Available online at www.sciencedirect.com Procedia Engineering 14 (2011) 2856 2863 The Twelfth East Asia-Pacific Conference on Structural Engineering and Construction Seismic Microzonation in Hurghada
More informationGlaciers and Glaciation
Chapter 18 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Glaciers and Glaciation Tarbuck and Lutgens Glaciers: A Part of Two Basic Cycles A glacier is a thick mass of ice that forms,
More informationSlot Couloir Accident, Snoqualmie Mt
Body Page 1 Slot Couloir Accident, Snoqualmie Mt 4-27-14 Date and Time: estimated 12 pm, Sunday 4/27/14 Location: Slot Couloir, Snoqualmie Mt Number in Party: 2 backcountry skiers Number hurt: 1 backcountry
More informationAssembly instructions for Eurotramp trampolines Series: Ultimate, Grand Master Exclusiv, Grand Master, Master
Assembly instructions for Eurotramp trampolines Series: Ultimate, Grand Master Exclusiv, Grand Master, Master 1. Assembly instructions 2. Attaching the plastic coated steel cables on the Ultimate frame
More informationIn southern Upper Valais a very high avalanche danger will be encountered in some regions Edition: , 08:00 / Next update: 9.1.
Page 1/6 In southern Upper Valais a very high avalanche danger will be encountered in some regions Edition: 9.1.2018, 08:00 / Next update: 9.1.2018, 17:00 Avalanche danger updated on 9.1.2018, 08:00 region
More informationMIÑO O AND LIMIA BASINS
Miño-Sil MIÑO O AND LIMIA BASINS José Álvarez Díaz Sil River Basin District s s Planning Office, Spain WORKSHOP ON TRANSBOUNDARY WATER RESOURCES BUDAPEST, HUNGARY, 8-10 FEBRUARY 2011 INDEX 1. OVERVIEW
More informationPOINT OF VIEW on the proposed solutions for improving navigation at critical points at Bechet, Corabia, Belene and Popina
FAST DANUBE C.N.F.R NAVROM S.A. Galaţi POINT OF VIEW on the proposed solutions for improving navigation at critical points at Bechet, Corabia, Belene and Popina 20.09.2018 Critical point from Bechet (km
More informationSHELTER DESIGN: IGLOO SNOW SHELTER
CONSTRUCTION: CHALLENGING 2 to 3 hours for two people. EQUIPMENT: Sawing instrument SEASON: Winter The Igloo shelter is not a shelter that should be built in an emergency situation as they are hard to
More informationSOME NEW STUDIES IN BINH CHAU GEOTHERMAL AREA, SOUTH VIETNAM
SOME NEW STUDIES IN BINH CHAU GEOTHERMAL AREA, SOUTH VIETNAM Nguyen Hong BANG and Nguyen Thac CUONG Division for Water Resources Planning and Investigation for the South of Vietnam 59 Street 2, Binh An
More informationREPORT OF STUDY TRIP (TOHOKU)
INTERNATIONAL INSTITUTE OF SEISMOLOGY AND EARTHQUAKE ENGINEERING (IISEE) REPORT OF STUDY TRIP (TOHOKU) 10-14 JULY 2011 PREPARED BY: MAZNI BINTI AZIS MALAYSIA SUBMISSION DATE: JULY 29, 2011 TSUNAMI DISASTER
More informationDid It. naturalists. Young. Moving and melting ice shaped many of Minnesota s land features. 30 Minnesota Conservation Volunteer
Young naturalists by Mary Hoff Photography by Gary Alan Nelson T he Glacier Did It Moving and melting ice shaped many of Minnesota s land features. Shut your eyes. Imagine that it s a sunny summer day
More informationLandscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age.
Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age. Key idea: Ice was a powerful force in shaping the landscape of the UK. As the climate has changed in the past,
More informationDETECTION OF ICE FRONT INITIATION ON THE PEACE RIVER IN NORTHERN ALBERTA Freeze-up
FINAL REPORT DETECTION OF ICE FRONT INITIATION ON THE PEACE RIVER IN NORTHERN ALBERTA Freeze-up 2013-2014 REFERENCE NO. CO 73797 Presented to: British Columbia Hydro and Power Authority Prepared by: Monique
More informationGLACIATION. The Last Ice Age (see Chapter 12) and. Pleistocene Ice Cap. Glacial Dynamics 10/2/2012. Laurentide Ice Sheet over NYS
GLACIATION and New York State Prof. Anthony Grande The Last Ice Age (see Chapter 1) The Pleistocene Epoch began 1.6 mya. During this time, climates grew colder. There were numerous ice ages starting 100,000000
More informationMeet the world s newest glacier at Mount St. Helens
Meet the world s newest glacier at Mount St. Helens By Seattle Times, adapted by Newsela staff on 08.10.15 Word Count 733 Hikers walk past this chunk of the volcano that existed before May 18, 1980. The
More informationGifts of the Glaciers
Gifts of the Glaciers Gifts of the Glaciers Moving ice of glacier was responsible for water, landforms, and soil characteristics and patterns of today Sculpturing of bedrock materials Glacial Landforms
More informationAvalanche Observations
Avalanche Observations Avalanche Observations 3.1 Introduction Observations of past and present avalanche activity are of the utmost importance for any avalanche forecasting operation. These data should
More informationQ: What is a period of time whereby the average global temperature has decreased? Q: What is a glacier?
Q: What is a glacier? A: A large sheet of ice which lasts all year round. Q: What is a period of time whereby the average global temperature has decreased? A: A glacial. Q: What is an interglacial? Q:
More informationLESOTHO HIGHLANDS DEVELOPMENT AUTHORITY
LESOTHO HIGHLANDS DEVELOPMENT AUTHORITY ANNUAL FLOW RELEASES INSTREAM FLOW REQUIREMENT (IFR) IMPLEMENTATION AND MONITORING (October 2005 to September 2006) REPORT N0.7 OCTOBER 2007 STRATEGIC AND CORPORATE
More informationTitle/Name of the area: Chwaka Bay, Zanzibar
Title/Name of the area: Chwaka Bay, Zanzibar Presented by: Dr. Charles Lugomela, Ag. Head, Department of Aquatic Sciences and Fisheries, University of Dar es Salaam, P.O. Box 35064 Dar es Salaam, Tanzania
More informationLesson. Glaciers Carve the Land A QUICK LOOK. Overview. Big Idea. Process Skills Key Notes
EARTH S CHANGING SURFACE CLUSTER 2 HOW THE EARTH S SURFACE CHANGES Lesson 62 Glaciers Carve the Land A QUICK LOOK Big Idea Moving water, ice, and wind break down rock, transport materials, and build up
More informationJust how big is Africa?
The United States China India The United Kingdom Portugal Spain France Belgium Germany The Netherlands Switzerland Italy Eastern Europe Japan 11.7 million sq. miles Just how big is Africa? Chapter 18 Section
More informationActive Glacier Protection in Austria - An adaptation strategy for glacier skiing resorts
in Austria - An adaptation strategy for glacier skiing resorts Presented by Marc Olefs Ice and Climate Group, Institute of Meteorology And Geophysics, University of Innsbruck Centre for Natural Hazard
More informationHydrology Baseline Report (all watercourses except Rivers Liakhvi and Supsa)
Section 3.2a Hydrology Baseline Report (all watercourses except Rivers Liakhvi and Supsa) NOTE: The survey was undertaken on a previous version of the route, therefore some of the crossings surveyed differ
More informationArchitectural Analysis in Western Palenque
Architectural Analysis in Western Palenque James Eckhardt and Heather Hurst During the 1999 season of the Palenque Mapping Project the team mapped the western portion of the site of Palenque. This paper
More informationUniversity of Rouen-Normandy, UMR CNRS 6014 COBRA, 55 rue Saint Germain, Evreux, France. 2
Long-term accumulation of metals and persistent pollutants (PAHs, PCBs, organochlorine pesticides) from Eure river watershed (France) in sediments: possible consequences of a dam removal THOMAS GARDES
More informationThe Yingtianmen Gate-site of the Sui and Tang Eastern Capital in Luoyang City
Nandajie The Yingtianmen Gate-site of the Sui and Tang Eastern Capital in Luoyang City Tang Luoyang City-site Archaeological Team, Institute of Archaeology, Chinese Academy of Social Sciences Key words:
More information