River Systems Earth Space Science Mr. Coyle The Hydrologic Cycle • Infiltration = Groundwater System • Runoff = Surface Water System • Runoff = Precipitation - Evapotranspiration Where is the Water ? RIVERS & STREAMS • • • • • • Water Reservoirs The Hydrologic Cycle Surface Water Systems Meandering Deltas/Alluvial Fans Floods and flooding Importance of rivers • Rivers: – – – – – Provide water and nutrients for agriculture Provide habitat to diverse flora and fauna Provide routes for commerce Provide recreation Provide electricity www.aquatic.uoguelph.ca/rivers/chintro.htm Natural Watercourses • Discharge- volume of water • Velocity- rate of water movement • Gradient- slope of inclined surface Variation in time and space • The shape, size and content of a river are constantly changing, forming a close and mutual interdependence between the river and the land it traverses. What is a Watershed? www.dec.state.ny.us/website/2000/watersheds.gif www.aquatic.uoguelph.ca/rivers/chwater.htm www.epa.gov/watertrain/ecology/ecology21.html L a rg e s t R iv e rs o f th e W o rld A p p r o x . le n g th R iv e r O u tflo w N ile M e d ite r r a n e a n S e a m i. 4 ,1 8 0 km 6 ,6 9 0 A m a z o n A tla n tic O c e a n 3 ,9 1 2 6 ,2 9 6 M is s is s ip p i-M is s o u r i G u lf o f M e x ic o 3 ,7 1 0 5 ,9 7 0 Y a n g tz e K ia n g C h in a S e a 3 ,6 0 2 5 ,7 9 7 O b G u lf o f O b 3 ,4 5 9 5 ,5 6 7 H u a n g H o (Y e llo w ) G u lf o f C h ih li 2 ,9 0 0 4 ,6 6 7 Y e n is e i A r c tic O c e a n 2 ,8 0 0 4 ,5 0 6 P a r a n á R ío d e la P la ta 2 ,7 9 5 4 ,4 9 8 2 ,7 5 8 4 ,4 3 8 2 ,7 1 6 4 ,3 7 1 2 ,7 0 4 4 ,3 5 2 2 ,6 5 2 4 ,2 6 8 2 ,6 3 5 4 ,2 4 1 N ig e r G u lf o f G u in e a 2 ,6 0 0 4 ,1 8 4 M e k o n g S o u th C h in a S e a 2 ,5 0 0 4 ,0 2 3 2 ,3 4 8 3 ,7 7 9 2 ,3 1 5 3 ,7 2 6 2 ,2 9 1 3 ,6 8 7 M a d e ir a A m a z o n R iv e r 2 ,0 1 2 3 ,2 3 8 P u r u s A m a z o n R iv e r 1 ,9 9 3 3 ,2 0 7 1 ,9 8 7 3 ,1 9 8 1 ,9 7 9 3 ,1 8 5 1 ,9 0 0 3 ,0 5 8 1 ,8 8 5 3 ,0 3 4 1 ,8 0 0 2 ,8 9 7 1 ,8 0 0 2 ,8 9 7 D a n u b e B la c k S e a 1 ,7 6 6 2 ,8 4 2 E u p h r a te s S h a tt-a l-A r a b 1 ,7 3 9 2 ,7 9 9 D a r lin g M u r r a y R iv e r 1 ,7 0 2 2 ,7 3 9 1 ,7 0 0 2 ,7 3 6 1 ,6 7 7 2 ,6 9 9 Ir tis h O b R iv e r Z a ir e (C o n g o ) A tla n tic O c e a n H e ilo n g (A m u r ) T a ta r S tr a it L e n a A r c tic O c e a n M a c k e n z ie B e a u fo r t S e a (A r c tic O c e a n ) M is s is s ip p i G u lf o f M e x ic o M is s o u r i M is s is s ip p i R iv e r V o lg a C a s p ia n S e a S ã o F r a n c is c o A tla n tic O c e a n Y u k o n B e r in g S e a S t. L a w r e n c e G u lf o f S t. L a w r e n c e R io G r a n d e G u lf o f M e x ic o B r a h m a p u tr a G a n g e s R iv e r In d u s A r a b ia n S e a Z a m b e z i M o z a m b iq u e C h a n n e l T o c a n tin s P a r á R iv e r The Worlds Largest Rivers Discharge River 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 Amazon, Brazil Congo, Zaire Yangtse Kiang, China Orinoco, Venezuela Brahmaputra, Bangladesh La Plata, Brazil Yenissei, Russia Mississippi, USA Lena, Russia Mekong, Vietnam Ganges, India Irrawaddy, Burma Ob, Russia Sikiang, China Amur, Russia St. Lawrence, Canada m^3/sec 190,000 42,000 35,000 29,000 20,000 19,500 17,800 17,700 16,300 15,900 15,500 14,000 12,500 11,500 11,000 10,400 % of total Runoff mm/yr entering Ratio oceans 835 340 560 845 1070 235 215 175 210 630 455 1020 135 840 190 310 13.0 2.9 2.4 2.0 1.4 1.3 1.2 1.2 1.1 1.1 1.1 1.0 0.9 0.8 0.8 0.7 0.47 0.25 0.50 0.46 0.65 0.20 0.42 0.21 0.46 0.43 0.42 0.60 0.24 0.32 0.33 U.S. Precipitation Map Notice the effect of the Rocky Mountains U.S. Runoff Map Laminar vs. Turbulent Flow Near-Laminar flow in the center of a river channel Turbulent flow in the headwaters of a rushing mountain stream So Where Does The Stream Move Fastest? • Headwaters move slowest • Mouth of stream moves fastest • Laminar flow is more efficient than turbulent flow. • Deeper stream move faster than shallow streams Sediment Load Movement of Bedload by Saltation Sedimentation Longitudinal Stream Profile Can be divided into 3 main parts Drainage (Tributary) Transport System Distributary System System Drainage System • Stream energy is spent eroding downward into the basement rock and... • Moving sediment • Creates “V” shaped canyon and valleys • When streams emerge from the mountain front, they often deposit some of this sediment forming alluvial fans. Alluvial Fans Transition from Tributary to Transport Aging Rivers: How Old Is It? • Young- rapid bed erosion, waterfalls, rapids, v-shaped valleys, few tributaries, low volume • Mature- well established tributaries, larger volume of water, erode banks and not the bed (bottom), meanders, oxbow lakes Flash Flooding & Sheetwash Braided Pattern = high slope + high stream power + coarse bed materials Braided Streams & Rivers • High sediment load • Constantly changing course • Floodplain is completely occupied by channels • Many small islands called mid-channel bars • Usually coarse sand and gravel deposits. Meandering Rivers Meandering Rivers • • • • Constantly erode material - Cut bank Constantly deposit material - Point bar Change their channel course gradually Create floodplains wider than the channel – Very Fertile soil – Subjected to seasonal flooding Formation of Meanders Point bar deposits Point Bar Deposits Point bar deposits grows laterally through time Cut bank erosion Point bar deposits } Meander loop Formation of an Oxbow Meandering stream flowing from top of screen to bottom Maximum deposition Maximum erosion Meander scars Oxbow Lake Oxbow cuttoff 1993 Mississippi Flood Flooding & Sedimentation Deltas - Distribution Systems If the Mississippi changes course again, what will happen to the City of New Orleans? Things to Remember • • • • Rivers are part of a larger hydrologic system The have three main components: Drainage (Tributary) systems - collect water Transport Systems - move water along – Alluvial fans, braided streams, meandering streams • Rivers exceed their capacity during floods • Distributary systems - return water to the sea – Deltas.