Rivers and Streams The Hydrologic Cycle Rivers and
- Slides: 72
Rivers and Streams The Hydrologic Cycle
Rivers and Streams Drainage basin or watershed
A River Mill Creek Drainage Basin
Walla. Basin Walla River Drainage Basin Mill Creek Drainage
Flow
Flow
Equilibrium and the longitudinal profile Gradient Velocity Discharge Q=Vx. A ft 3/sec (cfs) or m 3/sec (cms) V = velocity A = Cross-sectional area = Width x mean depth Base level (ultimate and local)Gradient Load
Velocity Variation
Variations with Discharge
Load
Load: Bed load (rolling, saltation) F Suspended load: silt and clay carried in suspension F Dissolved load: ions in solution HCO 3 - SO 42 - Ca 2+ Na+ Mg 2+ typically 90% of dissolved Competence: the amount of load that a particular stream can carry F
Load: Suspended Load
Load: Bed-load
2000 Hydrograph for Mill Creek at Walla Averages for 1942 -1990 1800 1600 Discharge (cfs) 1400 1200 1000 800 600 400 Maximum 200 Mean Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep
The Graded Stream The Longitudinal Profile
Braided/Meandering
Braided/Meandering
Velocity Variation
Meandering and Floodplains
Point Bar – Cut Bank
Point Bar – Cut Bank
Point Bar – Cut Bank
Point Bar – Cut Bank
Meandering and Floodplains
Meandering and Floodplains
Meandering and Floodplains
Meandering and Floodplains
Meandering and Floodplains
Meandering and Floodplains
Meandering and Floodplains
Deltas
Deltas
Deltas
Deltas
Deltas
Alluvial Fans
Floodplain Terraces
Floodplain Terraces
Stream Piracy
Flooding is dependent upon F precipitation in drainage basin F precipitation rate/infiltration rate F topography Flood Discharge = channel discharge when a river overflows its banks Flood Magnitude = discharge above flood discharge Flood Stage = elevation of water surface for a high-water condition likely to damage Thus depends on use of floodplain
Hydrograph for Mill Creek flood, Feb, 1996 Measured at Kooskie (max. was 6000 cfs at Walla) Mill Creek Flows 3500 Discharge (cfs) 3000 2500 2000 1500 1000 500 0 0 5 10 Day in Feb, 1996 15
Recurrence Interval as flood indicator Rec. Int. = (Y-1)/R Y = # of years for data R = rank of flood
Natural Levee
Response to Flood Hazards F Physical barriers · Levees · Flood walls with huge steel gates around towns · Retention reservoirs · Channelization to handle increase discharge · Storm channel system (LA)
Levees protect area behind until flood becomes too great working levee damming water behind it failed levee
Floodwalls on Mississippi in St. Louis and New Orleans
Flood Hazard Mapping Satellite images Upper = normal flow 1988 Lower = 1993 flooding
Landscape Evolution
- Water cycle the hydrologic cycle
- Bill nye rivers and streams
- Different bodys of water
- Why are some rivers in texas called “wrong way” rivers?
- Hydrologic routing and hydraulic routing
- Hydrologic engineering center
- Muskingum method
- Hydrologic routing
- Infiltration
- Hydrologic equation
- Hydrologic abstractions
- Objectiveable
- Hydrologic continuity equation
- Hydrologic engineering center
- Hydrograph
- River analysis system
- Hydrologic engineering center
- Female figure holding a fly-whisk
- Gulf stream
- Cost streams
- Oracle streams
- Groundwater table
- In the desert, ephemeral streams _____.
- Input output stream c++
- Data nugget streams as sensors answers
- 3 types of fire streams
- 3 types of fire streams
- Oracle streams
- Basic concepts in mining data streams
- A framework for clustering evolving data streams
- Streams anu
- 2140705
- Stream lazy evaluation
- Psychrometric processes
- Predefined streams in java
- High gradient stream
- Most streams carry the largest part of their load
- Once there were brook trout in the streams in the mountains
- Poetic techniques in the wild swans at coole
- Disappearing streams karst topography
- Vvvnn
- Finding frequent items in data streams
- Lego business model canvas
- Copy and paste
- Business key activities
- Perforce virtual streams
- Perforce virtual streams
- Discretized streams
- Cba streams
- There's a place where mercy reigns and never dies
- Hát kết hợp bộ gõ cơ thể
- Slidetodoc
- Bổ thể
- Tỉ lệ cơ thể trẻ em
- Voi kéo gỗ như thế nào
- Chụp phim tư thế worms-breton
- Chúa yêu trần thế alleluia
- Các môn thể thao bắt đầu bằng tiếng chạy
- Thế nào là hệ số cao nhất
- Các châu lục và đại dương trên thế giới
- Công thức tính thế năng
- Trời xanh đây là của chúng ta thể thơ
- Cách giải mật thư tọa độ
- Phép trừ bù
- độ dài liên kết
- Các châu lục và đại dương trên thế giới
- Thơ thất ngôn tứ tuyệt đường luật
- Quá trình desamine hóa có thể tạo ra
- Một số thể thơ truyền thống
- Cái miệng bé xinh thế chỉ nói điều hay thôi
- Vẽ hình chiếu vuông góc của vật thể sau
- Nguyên nhân của sự mỏi cơ sinh 8
- đặc điểm cơ thể của người tối cổ