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Mid-Holocene-to-present Modeled (ca., 7,000 to 100 cal. BP) and Reconstructed (ca., 5,900 to 5,436 cal. BP) Temperature for the High-Elevations of the Greater Yellowstone Ecosystem: Derived from a Transient Climate Model and Whitebark Pine Tree-rings
Research datakeyboard_double_arrow_right Dataset 2024 United States Publisher:U.S. Geological Survey
Authors: Gregory T Pederson; Nathan Chellman; Joseph McConnell; Cathy Whitlock; +8 Authors
Gregory T Pederson; Nathan Chellman; Joseph McConnell; Cathy Whitlock; Daniel Stahle; David McWethy; Matthew Toohey; Johann Jungclaus; Craig Lee; Justin T Martin; Mio Alt; Nickolas Kichas;
doi: 10.5066/p147tvzu
doi: 10.5066/p147tvzu
In the Rocky Mountains of the Greater Yellowstone Ecosystem (United States), recent melting at a high-elevation (3,091 m asl) ice patch exposed a mature stand of whitebark pine (Pinus albicaulis) trees located ~180 m above modern treeline dating to the mid-Holocene (c. 5,900-5,436 cal y BP +- 51 y). From this subfossil wood record, we contextualize the recent magnitude of warming relative to mid-Holocene conditions and reconstruct changes in climate that resulted in regional ice patch growth and reductions in treeline elevation. Specifically, we developed tree-ring based temperature estimates for subalpine treeline and compare and contextualize this record against a mid-Holocene-to-present (ca., 7,000 to 100 cal. BP) transient climate model.
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U.S. Geological Survey
Dataset . 2024
License: CC 0
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Mid-Holocene-to-present Modeled (ca., 7,000 to 100 cal. BP) and Reconstructed (ca., 5,900 to 5,436 cal. BP) Temperature for the High-Elevations of the Greater Yellowstone Ecosystem: Derived from a Transient Climate Model and Whitebark Pine Tree-rings
Research datakeyboard_double_arrow_right Dataset 2024 United States Publisher:U.S. Geological Survey
Authors: Gregory T Pederson; Nathan Chellman; Joseph McConnell; Cathy Whitlock; +8 Authors
Gregory T Pederson; Nathan Chellman; Joseph McConnell; Cathy Whitlock; Daniel Stahle; David McWethy; Matthew Toohey; Johann Jungclaus; Craig Lee; Justin T Martin; Mio Alt; Nickolas Kichas;
doi: 10.5066/p147tvzu
doi: 10.5066/p147tvzu
In the Rocky Mountains of the Greater Yellowstone Ecosystem (United States), recent melting at a high-elevation (3,091 m asl) ice patch exposed a mature stand of whitebark pine (Pinus albicaulis) trees located ~180 m above modern treeline dating to the mid-Holocene (c. 5,900-5,436 cal y BP +- 51 y). From this subfossil wood record, we contextualize the recent magnitude of warming relative to mid-Holocene conditions and reconstruct changes in climate that resulted in regional ice patch growth and reductions in treeline elevation. Specifically, we developed tree-ring based temperature estimates for subalpine treeline and compare and contextualize this record against a mid-Holocene-to-present (ca., 7,000 to 100 cal. BP) transient climate model.
U.S. Geological Surv...arrow_drop_down
U.S. Geological Survey
Dataset . 2024
License: CC 0
Data sources: Datacite
linkLink to
shareshareShare
citeCite
addClaim
Please grant OpenAIRE to access and update your ORCID works.
This Research product is the result of merged Research products in OpenAIRE.

You have already added works in your ORCID record related to the merged Research product.
This Research product is the result of merged Research products in OpenAIRE.

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0
citations 0
popularity Average
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Powered by BIP!
more_vert
U.S. Geological Surv...arrow_drop_down
U.S. Geological Survey
Dataset . 2024
License: CC 0
Data sources: Datacite
linkLink to
shareshareShare
citeCite
addClaim
Please grant OpenAIRE to access and update your ORCID works.
This Research product is the result of merged Research products in OpenAIRE.

You have already added works in your ORCID record related to the merged Research product.
This Research product is the result of merged Research products in OpenAIRE.

You have already added works in your ORCID record related to the merged Research product.
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Mid-Holocene-to-present Modeled (ca., 7,000 to 100 cal. BP) and Reconstructed (ca., 5,900 to 5,436 cal. BP) Temperature for the High-Elevations of the Greater Yellowstone Ecosystem: Derived from a Transient Climate Model and Whitebark Pine Tree-rings

Mid-Holocene-to-present Modeled (ca., 7,000 to 100 cal. BP) and Reconstructed (ca., 5,900 to 5,436 cal. BP) Temperature for the High-Elevations of the Greater Yellowstone Ecosystem: Derived from a Transient Climate Model and Whitebark Pine Tree-rings

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Mid-Holocene-to-present Modeled (ca., 7,000 to 100 cal. BP) and Reconstructed (ca., 5,900 to 5,436 cal. BP) Temperature for the High-Elevations of the Greater Yellowstone Ecosystem: Derived from a Transient Climate Model and Whitebark Pine Tree-rings

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Mid-Holocene-to-present Modeled (ca., 7,000 to 100 cal. BP) and Reconstructed (ca., 5,900 to 5,436 cal. BP) Temperature for the High-Elevations of the Greater Yellowstone Ecosystem: Derived from a Transient Climate Model and Whitebark Pine Tree-rings