 
Headwater Forests in Yellowstone National Park
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Forests in tributary headwaters are natural mechanisms for accumulating and retaining snow pack on windy ridges. As well, their shade and water-retentive roots create a more gradual release of snowpack melt downstream. However as climate change, mountain pine beetle attacks, high-intensity fire and timbering reduce forest acreage, downstream stakeholders will experience higher flooding with more intense spring snow melt followed by less water available thereafter when there’s no snow pack remaining to be released.
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Burned pine bark from 1988 fire 080601_WY_2529 |
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Burned pines, 1988 fire 080602_WY_6075 |
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Dead pine trunk from 1988 fire 080601_WY_5835 |
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Rotting, lichen-covered trunk 080530_WY_1691 |
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Windbreak of pines on ridge 080602_WY_2702 |
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Like fallen matchsticks after fire 080530_WY_1701 |
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Elk browse and fire threaten pines 080602_WY_6084 |
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Aspen tree 080530_WY_1713 |
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Higher elevation whitebark pine dying 080601_WY_5954 |
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Dead whitebark pine, likely beetle attack 080601_WY_5683 |
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Cottonwood copse in river valley 080602_WY_3132 |
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Pine silhouetted against cottonwood 080602_WY_2869 |
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