Climatic influences on hillslope soil transport efficiency
Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2014.
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| Format: | Thesis |
| Language: | eng |
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Massachusetts Institute of Technology
2014
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| Online Access: | http://hdl.handle.net/1721.1/90655 |
| _version_ | 1811090656366428160 |
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| author | Schurr, Naomi D. (Naomi Danika) |
| author2 | J. Taylor Perron. |
| author_facet | J. Taylor Perron. Schurr, Naomi D. (Naomi Danika) |
| author_sort | Schurr, Naomi D. (Naomi Danika) |
| collection | MIT |
| description | Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2014. |
| first_indexed | 2024-09-23T14:49:47Z |
| format | Thesis |
| id | mit-1721.1/90655 |
| institution | Massachusetts Institute of Technology |
| language | eng |
| last_indexed | 2024-09-23T14:49:47Z |
| publishDate | 2014 |
| publisher | Massachusetts Institute of Technology |
| record_format | dspace |
| spelling | mit-1721.1/906552019-04-12T13:31:23Z Climatic influences on hillslope soil transport efficiency Schurr, Naomi D. (Naomi Danika) J. Taylor Perron. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Earth, Atmospheric, and Planetary Sciences. Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2014. Cataloged from PDF version of thesis. Includes bibliographical references (pages 36-38). The soil transport coefficient D represents the relationship between local topographical gradient and soil flux in the landscape evolution model. This work presents new estimates of the soil transport coefficient D at 9 sites and compares them, along with a compilation of 16 previously published estimates of D, against three climate proxies (mean annual precipitation, aridity index, and mean annual temperature) with the goal of characterizing climatic influences on soil transport efficiency. The new measurements were performed at sites that extend the range into both drier and wetter climates than those published. Together the data suggest that D increases with mean annual precipitation and aridity in dry climates, and levels off or decreases gradually in wetter climates. by Naomi D. Schurr. S.B. 2014-10-08T15:20:48Z 2014-10-08T15:20:48Z 2014 2014 Thesis http://hdl.handle.net/1721.1/90655 890396278 eng M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 64 pages application/pdf Massachusetts Institute of Technology |
| spellingShingle | Earth, Atmospheric, and Planetary Sciences. Schurr, Naomi D. (Naomi Danika) Climatic influences on hillslope soil transport efficiency |
| title | Climatic influences on hillslope soil transport efficiency |
| title_full | Climatic influences on hillslope soil transport efficiency |
| title_fullStr | Climatic influences on hillslope soil transport efficiency |
| title_full_unstemmed | Climatic influences on hillslope soil transport efficiency |
| title_short | Climatic influences on hillslope soil transport efficiency |
| title_sort | climatic influences on hillslope soil transport efficiency |
| topic | Earth, Atmospheric, and Planetary Sciences. |
| url | http://hdl.handle.net/1721.1/90655 |
| work_keys_str_mv | AT schurrnaomidnaomidanika climaticinfluencesonhillslopesoiltransportefficiency |