TY - JOUR
T1 - Plants in water-controlled ecosystems
T2 - Active role in hydrologic processes and responce to water stress IV. Discussion of real cases
AU - Laio, F.
AU - Porporato, Amilcare Michele M.
AU - Fernandez-Illescas, C. P.
AU - Rodriguez-Iturbe, I.
N1 - Funding Information:
We are grateful to the Central Plains Experimental Range (CPER) for providing the rainfall data for the Colorado steppe application. This paper was partially funded by the National Science Foundation grants EAR-9996180 and EAR-9705861.
PY - 2001/7
Y1 - 2001/7
N2 - Three water-controlled ecosystems are studied here using the stochastic description of soil moisture dynamics and vegetation water stress proposed in Part II (F. Laio, A. Porporato, L. Ridolfi, I. Rodriguez-Iturbe, Adv. Water Res. 24 (7) (2001) 707-723) and Part III (A. Porporato, F. Laio, L. Ridolfi, I. Rodriguez-Iturbe, Adv. Water Res. 24 (7) (2001) 725-744) of this series of papers. In the savanna of Nylsvley (South Africa) the very diverse physiological characteristics of the existing plants give rise to different strategies of soil moisture exploitation. Notwithstanding these differences, the vegetation water stress for all the species turns out to be very similar, suggesting that coexistence might be attained also through differentiation of water use. The case of the savanna of Southern Texas points out how rooting depth and interannual rainfall variability can impact soil moisture dynamics and vegetation water stress. Because of the different responses to water stress of trees and grasses, external climatic forcing could be at the origin of the dynamic equilibrium allowing coexistence in this ecosystem. Finally, the analysis of a short grass steppe in Colorado provides an interesting example of the so-called inverse texture effect, whereby preferential conditions for vegetation are dependent on soil texture and rainfall. Sites which are more favorable during wet conditions may become less suitable to the same vegetation type during drier years. Such an effect is important to explain the predominance of existing species, as well as to investigate their reproductive strategies.
AB - Three water-controlled ecosystems are studied here using the stochastic description of soil moisture dynamics and vegetation water stress proposed in Part II (F. Laio, A. Porporato, L. Ridolfi, I. Rodriguez-Iturbe, Adv. Water Res. 24 (7) (2001) 707-723) and Part III (A. Porporato, F. Laio, L. Ridolfi, I. Rodriguez-Iturbe, Adv. Water Res. 24 (7) (2001) 725-744) of this series of papers. In the savanna of Nylsvley (South Africa) the very diverse physiological characteristics of the existing plants give rise to different strategies of soil moisture exploitation. Notwithstanding these differences, the vegetation water stress for all the species turns out to be very similar, suggesting that coexistence might be attained also through differentiation of water use. The case of the savanna of Southern Texas points out how rooting depth and interannual rainfall variability can impact soil moisture dynamics and vegetation water stress. Because of the different responses to water stress of trees and grasses, external climatic forcing could be at the origin of the dynamic equilibrium allowing coexistence in this ecosystem. Finally, the analysis of a short grass steppe in Colorado provides an interesting example of the so-called inverse texture effect, whereby preferential conditions for vegetation are dependent on soil texture and rainfall. Sites which are more favorable during wet conditions may become less suitable to the same vegetation type during drier years. Such an effect is important to explain the predominance of existing species, as well as to investigate their reproductive strategies.
KW - Crossing analysis
KW - Ecohydrology
KW - Grasslands
KW - Hydrology
KW - Savannas
KW - Soil moisture
KW - Stochastic processes
KW - Vegetation
KW - Water balance
KW - Water stress
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U2 - 10.1016/S0309-1708(01)00007-0
DO - 10.1016/S0309-1708(01)00007-0
M3 - Article
AN - SCOPUS:0035398610
SN - 0309-1708
VL - 24
SP - 745
EP - 762
JO - Advances in Water Resources
JF - Advances in Water Resources
IS - 7
ER -