A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution
The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Jing [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Rechteinformationen: |
Nutzungsrecht: © 2017 Informa UK Limited, trading as Taylor & Francis Group 2017 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Physical geography - London [u.a.] : Taylor & Francis, 1980, 38(2017), 3, Seite 231-17 |
|---|---|
| Übergeordnetes Werk: |
volume:38 ; year:2017 ; number:3 ; pages:231-17 |
| Links: |
|---|
| DOI / URN: |
10.1080/02723646.2017.1281013 |
|---|
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| 520 | |a The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. | ||
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| 650 | 4 | |a mass elevation effect | |
| 650 | 4 | |a air temperature rise | |
| 650 | 4 | |a treeline | |
| 650 | 4 | |a Rocky Mountains | |
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10.1080/02723646.2017.1281013 doi PQ20170501 (DE-627)OLC1992729263 (DE-599)GBVOLC1992729263 (PRQ)c1269-64b9af950e9b6ca016f7df86eb15d3b35731ce485becd8de3032fca0ce85b8b20 (KEY)0103583520170000038000300231quantitativestudyonthemasselevationeffectoftherock DE-627 ger DE-627 rakwb eng 550 DNB 74.00 bkl 38.00 bkl Wang, Jing verfasserin aut A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. Nutzungsrecht: © 2017 Informa UK Limited, trading as Taylor & Francis Group 2017 mass elevation effect air temperature rise treeline Rocky Mountains Zhang, Baiping oth He, Wenhui oth Yao, Yonghui oth Zhang, Wenjie oth Zhao, Chao oth Enthalten in Physical geography London [u.a.] : Taylor & Francis, 1980 38(2017), 3, Seite 231-17 (DE-627)130506664 (DE-600)762499-2 (DE-576)016083776 0272-3646 nnns volume:38 year:2017 number:3 pages:231-17 http://dx.doi.org/10.1080/02723646.2017.1281013 Volltext http://www.tandfonline.com/doi/abs/10.1080/02723646.2017.1281013 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_24 GBV_ILN_2003 GBV_ILN_4082 GBV_ILN_4126 74.00 AVZ 38.00 AVZ AR 38 2017 3 231-17 |
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10.1080/02723646.2017.1281013 doi PQ20170501 (DE-627)OLC1992729263 (DE-599)GBVOLC1992729263 (PRQ)c1269-64b9af950e9b6ca016f7df86eb15d3b35731ce485becd8de3032fca0ce85b8b20 (KEY)0103583520170000038000300231quantitativestudyonthemasselevationeffectoftherock DE-627 ger DE-627 rakwb eng 550 DNB 74.00 bkl 38.00 bkl Wang, Jing verfasserin aut A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. Nutzungsrecht: © 2017 Informa UK Limited, trading as Taylor & Francis Group 2017 mass elevation effect air temperature rise treeline Rocky Mountains Zhang, Baiping oth He, Wenhui oth Yao, Yonghui oth Zhang, Wenjie oth Zhao, Chao oth Enthalten in Physical geography London [u.a.] : Taylor & Francis, 1980 38(2017), 3, Seite 231-17 (DE-627)130506664 (DE-600)762499-2 (DE-576)016083776 0272-3646 nnns volume:38 year:2017 number:3 pages:231-17 http://dx.doi.org/10.1080/02723646.2017.1281013 Volltext http://www.tandfonline.com/doi/abs/10.1080/02723646.2017.1281013 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_24 GBV_ILN_2003 GBV_ILN_4082 GBV_ILN_4126 74.00 AVZ 38.00 AVZ AR 38 2017 3 231-17 |
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10.1080/02723646.2017.1281013 doi PQ20170501 (DE-627)OLC1992729263 (DE-599)GBVOLC1992729263 (PRQ)c1269-64b9af950e9b6ca016f7df86eb15d3b35731ce485becd8de3032fca0ce85b8b20 (KEY)0103583520170000038000300231quantitativestudyonthemasselevationeffectoftherock DE-627 ger DE-627 rakwb eng 550 DNB 74.00 bkl 38.00 bkl Wang, Jing verfasserin aut A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. Nutzungsrecht: © 2017 Informa UK Limited, trading as Taylor & Francis Group 2017 mass elevation effect air temperature rise treeline Rocky Mountains Zhang, Baiping oth He, Wenhui oth Yao, Yonghui oth Zhang, Wenjie oth Zhao, Chao oth Enthalten in Physical geography London [u.a.] : Taylor & Francis, 1980 38(2017), 3, Seite 231-17 (DE-627)130506664 (DE-600)762499-2 (DE-576)016083776 0272-3646 nnns volume:38 year:2017 number:3 pages:231-17 http://dx.doi.org/10.1080/02723646.2017.1281013 Volltext http://www.tandfonline.com/doi/abs/10.1080/02723646.2017.1281013 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_24 GBV_ILN_2003 GBV_ILN_4082 GBV_ILN_4126 74.00 AVZ 38.00 AVZ AR 38 2017 3 231-17 |
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10.1080/02723646.2017.1281013 doi PQ20170501 (DE-627)OLC1992729263 (DE-599)GBVOLC1992729263 (PRQ)c1269-64b9af950e9b6ca016f7df86eb15d3b35731ce485becd8de3032fca0ce85b8b20 (KEY)0103583520170000038000300231quantitativestudyonthemasselevationeffectoftherock DE-627 ger DE-627 rakwb eng 550 DNB 74.00 bkl 38.00 bkl Wang, Jing verfasserin aut A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. Nutzungsrecht: © 2017 Informa UK Limited, trading as Taylor & Francis Group 2017 mass elevation effect air temperature rise treeline Rocky Mountains Zhang, Baiping oth He, Wenhui oth Yao, Yonghui oth Zhang, Wenjie oth Zhao, Chao oth Enthalten in Physical geography London [u.a.] : Taylor & Francis, 1980 38(2017), 3, Seite 231-17 (DE-627)130506664 (DE-600)762499-2 (DE-576)016083776 0272-3646 nnns volume:38 year:2017 number:3 pages:231-17 http://dx.doi.org/10.1080/02723646.2017.1281013 Volltext http://www.tandfonline.com/doi/abs/10.1080/02723646.2017.1281013 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_24 GBV_ILN_2003 GBV_ILN_4082 GBV_ILN_4126 74.00 AVZ 38.00 AVZ AR 38 2017 3 231-17 |
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10.1080/02723646.2017.1281013 doi PQ20170501 (DE-627)OLC1992729263 (DE-599)GBVOLC1992729263 (PRQ)c1269-64b9af950e9b6ca016f7df86eb15d3b35731ce485becd8de3032fca0ce85b8b20 (KEY)0103583520170000038000300231quantitativestudyonthemasselevationeffectoftherock DE-627 ger DE-627 rakwb eng 550 DNB 74.00 bkl 38.00 bkl Wang, Jing verfasserin aut A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. Nutzungsrecht: © 2017 Informa UK Limited, trading as Taylor & Francis Group 2017 mass elevation effect air temperature rise treeline Rocky Mountains Zhang, Baiping oth He, Wenhui oth Yao, Yonghui oth Zhang, Wenjie oth Zhao, Chao oth Enthalten in Physical geography London [u.a.] : Taylor & Francis, 1980 38(2017), 3, Seite 231-17 (DE-627)130506664 (DE-600)762499-2 (DE-576)016083776 0272-3646 nnns volume:38 year:2017 number:3 pages:231-17 http://dx.doi.org/10.1080/02723646.2017.1281013 Volltext http://www.tandfonline.com/doi/abs/10.1080/02723646.2017.1281013 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_24 GBV_ILN_2003 GBV_ILN_4082 GBV_ILN_4126 74.00 AVZ 38.00 AVZ AR 38 2017 3 231-17 |
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quantitative study on the mass elevation effect of the rocky mountains and its significance for treeline distribution |
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A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution |
| abstract |
The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. |
| abstractGer |
The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. |
| abstract_unstemmed |
The Rocky Mountains are the highest and most extensive in North America. Their mass-elevation effect (MEE) should be strong and responsible for the high elevations of treelines in the interior of the mountain range. However, the MEE has been little known. We calculated the temperature difference (ΔT) between the inner and outer Rocky Mountains at the same elevation and defined it as the magnitude of MEE. Results show a mean ΔT of 1.8°C, with the highest ΔT occurring in Colorado and the basins of southern Wyoming. The MEE can be modelled with three factors: mountain base elevation (MBE), latitude, and hygric continentality. The model has a high explanatory power of 68.90%, and the three factors contribute 45.65, 36.05, and 18.03%, respectively. MBE contributed most to MEE, both in the whole range (45.65%) and in the Colorado Rocky Mountains (55.21%). Treeline is higher in the interior than the outside of the mountain range, by 700-1400 m. This difference coincides well with air temperature differences. This study developed a quantitative model for the MEE of the Rocky Mountains and improves our understanding of the intra-mountain ecology and high treelines of the Rocky Mountains. |
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A quantitative study on the mass elevation effect of the Rocky Mountains and its significance for treeline distribution |
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