The role of topography in the emergence of African savannas

Includes bibliographical references (leaves 93-96). === Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2003. === The coexistence of trees and grasses in savannas are not well understood even though savannas occupy a wide area of West Africa. In th...

Full description

Bibliographic Details
Main Author: Kim, Yeonjoo, 1977-
Other Authors: Elfaith A.B. Eltahir.
Format: Others
Language:English
Published: Massachusetts Institute of Technology 2009
Subjects:
Online Access:http://hdl.handle.net/1721.1/44515
id ndltd-MIT-oai-dspace.mit.edu-1721.1-44515
record_format oai_dc
spelling ndltd-MIT-oai-dspace.mit.edu-1721.1-445152019-05-02T16:01:58Z The role of topography in the emergence of African savannas Kim, Yeonjoo, 1977- Elfaith A.B. Eltahir. Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. Civil and Environmental Engineering. Includes bibliographical references (leaves 93-96). Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2003. The coexistence of trees and grasses in savannas are not well understood even though savannas occupy a wide area of West Africa. In this study, a hypothesis is proposed to investigate the question of how trees and grasses coexist in a region. The hypothesis suggests that the variation in elevation leads to the variation in soil moisture, which in turn can explain the coexistence of trees and grasses in savannas. To test this hypothesis, experimental simulations are performed using biospheric model, IBIS, and distributed hydrologic model, SHE. We, first, estimate the amount of rainfall required for trees and grasses under a certain atmospheric condition. Here, the variation of rainfall is prescribed to force a similar variation of soil moisture. A 30% decrease in rainfall is sufficient to simulate grasses at 9°N. A 100% increase in rainfall is sufficient to simulate trees at II°N. However, even with a five fold increase in rainfall, the model fails to simulate trees at 13°N. To study the influences of topography explicitly, a distributed hydrologic modeling is performed using SHE. The results suggest that the variation of the depth to water table induced by the varying elevation is highly correlated with the variation of soil moisture. Consequently, an asynchronous coupling of SHE and IBIS is designed to investigate the stated hypothesis. The coupling is performed by modifying IBIS to include the groundwater table as a boundary variable. The modified IBIS simulates both trees and grasses according to a different water table boundary condition in natural savannas of 11°N. The shallow water table of valleys allows the growth of trees, and the deep water table of hills allows the growth of grasses. The simulations in this study suggest that the variability of soil moisture resulting from the topographic variation can be a determinant of savanna ecosystems. Moreover, grasslands in 13°N cannot be changed into forests only by adjusting soil moisture. It suggests that the role of soil moisture can be significant to dictate the vegetation type only in a certain window characteristic of savanna climate. by Yeonjoo Kim. S.M. 2009-01-30T16:55:26Z 2009-01-30T16:55:26Z 2003 2003 Thesis http://hdl.handle.net/1721.1/44515 54516529 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 96 leaves application/pdf fw----- Massachusetts Institute of Technology
collection NDLTD
language English
format Others
sources NDLTD
topic Civil and Environmental Engineering.
spellingShingle Civil and Environmental Engineering.
Kim, Yeonjoo, 1977-
The role of topography in the emergence of African savannas
description Includes bibliographical references (leaves 93-96). === Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2003. === The coexistence of trees and grasses in savannas are not well understood even though savannas occupy a wide area of West Africa. In this study, a hypothesis is proposed to investigate the question of how trees and grasses coexist in a region. The hypothesis suggests that the variation in elevation leads to the variation in soil moisture, which in turn can explain the coexistence of trees and grasses in savannas. To test this hypothesis, experimental simulations are performed using biospheric model, IBIS, and distributed hydrologic model, SHE. We, first, estimate the amount of rainfall required for trees and grasses under a certain atmospheric condition. Here, the variation of rainfall is prescribed to force a similar variation of soil moisture. A 30% decrease in rainfall is sufficient to simulate grasses at 9°N. A 100% increase in rainfall is sufficient to simulate trees at II°N. However, even with a five fold increase in rainfall, the model fails to simulate trees at 13°N. To study the influences of topography explicitly, a distributed hydrologic modeling is performed using SHE. The results suggest that the variation of the depth to water table induced by the varying elevation is highly correlated with the variation of soil moisture. Consequently, an asynchronous coupling of SHE and IBIS is designed to investigate the stated hypothesis. The coupling is performed by modifying IBIS to include the groundwater table as a boundary variable. The modified IBIS simulates both trees and grasses according to a different water table boundary condition in natural savannas of 11°N. The shallow water table of valleys allows the growth of trees, and the deep water table of hills allows the growth of grasses. The simulations in this study suggest that the variability of soil moisture resulting from the topographic variation can be a determinant of savanna ecosystems. Moreover, grasslands in 13°N cannot be changed into forests only by adjusting soil moisture. It suggests that the role of soil moisture can be significant to dictate the vegetation type only in a certain window characteristic of savanna climate. === by Yeonjoo Kim. === S.M.
author2 Elfaith A.B. Eltahir.
author_facet Elfaith A.B. Eltahir.
Kim, Yeonjoo, 1977-
author Kim, Yeonjoo, 1977-
author_sort Kim, Yeonjoo, 1977-
title The role of topography in the emergence of African savannas
title_short The role of topography in the emergence of African savannas
title_full The role of topography in the emergence of African savannas
title_fullStr The role of topography in the emergence of African savannas
title_full_unstemmed The role of topography in the emergence of African savannas
title_sort role of topography in the emergence of african savannas
publisher Massachusetts Institute of Technology
publishDate 2009
url http://hdl.handle.net/1721.1/44515
work_keys_str_mv AT kimyeonjoo1977 theroleoftopographyintheemergenceofafricansavannas
AT kimyeonjoo1977 roleoftopographyintheemergenceofafricansavannas
_version_ 1719033405858906112