Mammoth Caves National Park, Kentucky A collection of webcams of the Green River showing changes that occur on the landscape scale throughout a year (from.

Slides:



Advertisements
Similar presentations
Standard Workflow Scheme v2.0. This is an interactive presentation of the Standard Workflow Scheme v2.0. Feel free to click on the boxes to see the possible.
Advertisements

GEOGRAPHIC INFORMATION SYSTEM (GIS) AND REMOTE SENSING Lecture 4 Zakaria Khamis.
Equator Tropic of Cancer AFRICA ASIA Latitudes near the North Pole NORTH AMERICA We will examine a set of images and maps produced by NASA (vegetation.
Chapter 9 Water Erosion and Deposition
Running Water.
Climate Change: Past, Present and Future. Warm up: 1.Sketch a graph (Global Temperature vs. Time) for the past 20,000 years and predict how climate has.
Ecological Succession -may result from natural orderly changes, or from rapid changes due to disasters, such as fire, etc. -succession occurs as a series.
Measuring infiltration: Mm decline in level Minutes The water rapidly leaks away into the pore spaces in the soil. Rate of infiltration.
1. Sunshine (solar energy) 2. Rainfall 3. Temperature 4. Soil.
Wetlands Forests Deserts
Changing Colorful Leaves
Eclipses and Tides 6.E.1.1 Explain how the relative motion and relative position of the sun, Earth and moon affect the seasons,
FLOOD HYDROGRAPHS FOR GCSE GEOGRAPHY.
Chapter Soil Chapter 12.4 Soil as a Resource
What are the different biomes of the world?
Where Living Things are Found.
Succession Where the changing of species composition occurs over a period of time. Two main types: Primary succession: starting from scratch. Where there.
Surface Water Chapter 9.
Biomes are a group of ecosystems with similar abiotic and biotic factors. (example: hot/dry desert in Nevada and North Africa)
Chapter 4: Kinds of Ecosystems Section. 4.1: Forests.
Erosion by Glaciers. A glacier is Any large mass of ice that moves slowly over land Think of it as a moving river of ice and snow.
Run Off Water. Run off water is a result of water not being able to be absorbed by the surface of the ground. Gravity pulls the run off water along the.
Unit 7 – Bear Meadows, The Rockies and Greenland What do Rocky Mountain, Bear Meadows, and Greenland have in common? Hint: It’s cold up there on top of.
Preview: Biomes How do you think climate effects what vegetation and animals are in a region or area? It will effect the size of the population that supported.
‘A Question of’ …Nine Number Picture Boards This nine number picture board is adapted from a template available from
 Average rainfall: 29.5 inches  Average Temperatures in Summer: 82.4° F  Average Temperatures in Winter: 42.8°F.
Toronto’s Rivers Come Alive in 2005! ~ Edwards Gardens ~ M. Beukeboom.
SOLHEIMAJÖKULL FROM 1998 TO Solheimajökull is an outlet glacier from the Mýrdalsjökull ice cap. Under the ice cap is the volcano Katla which erupts.
1 Ecological Succession Change over time 1. 2 Pioneer Organisms Pioneer organisms are the first organisms to reoccupy an area which has been disturbed.
This house sits on the top of a hill that is covered with loose soil and rocks. The new owners of this house have some concerns about their property. What.
Unit 8 – Coasts & Sea-level Changes (Cape Cod & Acadia) Coasting Down the Coast.
PHS 120 TOPOGRAPHIC MAP BASICS
Unit 1 Lesson 3 Erosion and Deposition by Water
Poison Ivy Teaching Example/Non-Example. Performance Objective Students will be able to identify the difference between Poison Ivy from other types of.
Leaves Through the Seasons Produced by: Kylee and Julianne Winter Show the trees that have no leaves and explain why. Show the bare trees. Spring Showcase.
Natural Riparian Resources Water Landscape & SoilVegetation.
Summer, Autumn, Spring. Spring Sprig I love very much. Spring is the season after winter and before summer. Days become longer and weather gets warmer.
In this presentation you will: Ecological Succession explore the role of ecological succession Next > SoilGrassShrubs Small Trees Large Trees.
Water Erosion “We’re changing Earth’s Surface!” A. Stream Erosion 1. Running Water 2. Energy 3. The water cycle -Most effective agent in wearing down.
Changes to Earth’s Surface.  The surface of the Earth is constantly changing. Some changes happen quickly and can be dangerous. Others happen so slowly,
Rock Slide—Palisades Cliffs May 12, 2012 Images and “Why it Happened”
Observation Journal 8 weeks of wonder By Shannon Kelly.
The Big Storm: a satellite view of the channel In the three weeks following Christmas 2004, the South Coast was hit with a series of major winter storms.
BIOMES. Tropical Rain Forests Amazon in South America Located within 10 degrees of the equator Warm temperatures and heavy rainfall Rain exceedes evaporation.
Summer The leaves are green on the trees.
7th Grade Earth Space Science Quarterly Assessment
Ecological Succession
Red Maple by Noble High School.
Changes Through the Seasons
East Asia—Climate and Vegetation
Vincent Van Gogh’s Trees. Vincent Van Gogh’s Trees.
Vincent Van Gogh Trees.
January 14, 2013 Class : Table of contents: pg 9
Ground Water Dynamics.
Ground Water Dynamics.
A little brown acorn fell down to the ground, one windy and wet autumn day. and right there, he decided to stay. The dry leaves quickly covered him.
Do Now: Fire as an Ecological Disturbance
EARTH’S WATER SUPPLY.
Remote Sensing Ices on Mars
Seasons November 15, 2018.
Chapter 9 Water Erosion and Deposition
Species richness is the number of species in a community
Take Notes as you view the slides
Mammoth Caves National Park, Kentucky
Water as a Resource Rippling Water (Basic)
Water as a Resource Subtitle Here Rippling Water (Basic)
How do the four seasons effect the Weather?
NASA Images & MAPS We will examine a set of images and maps produced by NASA (vegetation images, land cover and population maps) and we will look for connections.
Interpreting Arial Photos
Click on one of the following icons to go to that resource.
Presentation transcript:

Mammoth Caves National Park, Kentucky A collection of webcams of the Green River showing changes that occur on the landscape scale throughout a year (from July 2007 to June 2008) Teacher’s version: Includes narrative indicating what changes are visible between webcam images.

Vegetation growing on the sandbars in the river Little distinction can be made between the different tree species during the summer. Trees that frame the webcam are deciduous but other species are presently indistinguishable. Sandbar outlined to show the change in size over next several slides, indicating a change in the discharge

Vegetation continues to grow on the sandbars Outlined sandbar is less exposed, indicating a rise in the water level (increase in discharge) River color is still the same as the last image – river sediment has not changed

The sandbars in the river are at their greatest extent – river water level (discharge) is low Trees growing on the right slope are in the beginning stages of changing color Some haze in sky (notice clearness on next slide)

Black line drawn on river marks the extent of the sandbar on the previous slide

Leaves are starting to change

Distinct leave color change

Noticeable differences in color Water level as indicated by the bank Vegetation on sandbar has changed to a brownish green color, another indication of the changing seasons

4 days after the last image Heavy amounts of sediment in river - evidenced by rich brown color Water level

Water level dropped – bank edge is visible (arrow) Less sediment in river – color returning to a greenish hue

Change of seasons makes it easier to see the complex series of slopes (drawn with black lines) within the valley Water level continues to drop – bank edge Re-emergence of sand bar in river, indicating drop in water level Bare trees evident

Note different species of trees, based on leaf color Continued water level drop and emergence of secondary sand bar

Increase in water level, gravel bars immersed Deep red and orange leaves are most prominent now

Near absence of deciduous leaves remaining on trees

Evergreen trees are only trees left with leaves

The river is noticeably greener indicating less sediment Gravel bars are also re-emerging

River flooding with a high sediment load caused the river to turn a sandy brown color The river is out of its bank with tree trunks in the water

The extent of the flooding increased from the last slide as more trees are now inundated with flood waters

A light covering of snow on the ground illustrates the extent of the flood

15 days after the last image: Flood waters have decreased River is returning to a green hue

A heavier snowfall this time: again indicating the extent of flooding

The greatest flood event witnessed over a 12 month period with the flood waters at its greatest extent out of its banks

Receding flood waters and a return of the natural color of the river A slight trace of spring green up can be found (arrow)

River is flooding again Spring green-up has begun Note the budding of the tree in the foreground over the next several images (arrow)

Pink buds are fading, to be replaced with leaves over the next several images

Gravel bars just beneath surface, general outline visible

Re-emergence of gravel bars

Submergence of gravel bars due to flooding Note high sediment load of river, evident from water color

The camera angle was adjusted slightly between May 3 rd and May 6 th (this webcam image). The flood waters have receded slightly (bank is visible (right arrow) Tree in foreground continues to leaf-out (left arrow).

Evidence of a recent flood is no longer visible in this image: the river is, once again, a greenish hue, the bank is visible, and sand bars in the middle of the river are slowly being exposed

The extent of sandbar exposure is similar to last year’s webcam image, indicating it is probably normal in the summer months