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Week 2: Yellowstone Sphere to Sphere Interactions
Below are some of the sphere > sphere interactions that could have occurred during the ESS analysis of the Yellowstone forest fires event.

Pay attention to how the "Why?" or "How?" for the interactions is made visible in the examples below. Make the “why” and “how” visible in your interactions by including, “What you really believe to be true, ‘I think...’” supported by reasons, “Because...” and, when possible, including "These reasons come from..."

Lithosphere and Biosphere

L > B
Burned plant debris that did not blow away becomes the new soil that can provide some nutrients for pioneer plants. By comparison, gardeners prepare their soil with ashes from a fireplace.

B > L
A decrease in vegetation may have resulted in increased erodibility of soil because there were fewer roots to hold the soil in place. In the area where I live, the roots from good plant cover appear to help keep the topsoil from washing away during heavy rains.

Lithosphere and Hydrosphere

L > H
Erosion increases from runoff following the fire and changes the turbidity, temperature, and pH of the streams and rivers. A similar circumstance occurs in the strip mining areas near where I live. Following hard rains, the nearby streams become very muddy. An article in the local paper said such "erosion and drainage creates acidic conditions in the streams."

Lithosphere and Atmosphere

L > A
Blackened areas can absorb heat faster, increasing the rate of convection in cells. An increase in convection may move air masses through a burned area quicker and/or cause moist air to move vertically faster, increasing rain further downwind.

A > L
Ash particles in the air could have been carried by the wind and dropped on the ground miles away from the forest fires; the ash particles--which have a high pH--could have changed the pH of the soil.

Atmosphere and Hydrosphere

A > H
Ash may be carried by winds many miles from the fire and then dropped into streams. A similar thing happens when ash from an erupting volcano is carried by the winds to other regions.

A > H
There may have been more precipitation in neighboring areas because ash particles in the air could have become condensation centers upon which raindrops could form.

Atmosphere and Biosphere

A > B
Smoke and noxious fumes could have coated the lungs of
animals and people, affecting their ability to breathe. 

A > B > E
I read that more than eight weeks of warm to hot, low humidity air masses drew moisture out of grasses and trees in Yellowstone National Park prior to the 1988 fires.

Biosphere and Hydrosphere

B > H
Destruction of waterside habitat (and cover) can raise water temperatures because the ponds and streams are exposed to more radiant energy from the sun.

[ Back to The Integration of the ESS Analysis and the PBL Model ]

[ Go to Yellowstone Event to Sphere Interactions ]

[ Go to Yellowstone Causal Chains ]

[ Back to Outline ]


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