Water-limited vegetated ecosystems driven by stochastic rainfall: feedbacks and bimodality

被引:2
|
作者
Schaffer, Benjamin E. [1 ]
Rodriguez-Iturbe, Ignacio [1 ,2 ,3 ,4 ]
机构
[1] Princeton Univ, Dept Civil & Environm Engn, Princeton, NJ 08540 USA
[2] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX 77843 USA
[3] Texas A&M Univ, Dept Ocean Engn, College Stn, TX 77843 USA
[4] Texas A&M Univ, Dept Civil Engn, College Stn, TX 77843 USA
基金
美国国家科学基金会;
关键词
stochastic process; soil moisture; biomass; ecohydrology; bimodality; vegetation feedbacks; SOIL-MOISTURE; HYDROLOGIC PROCESSES; SELF-ORGANIZATION; ACTIVE-ROLE; MODEL; DYNAMICS; PATTERNS; PLANTS; SYSTEMS; CLIMATE;
D O I
10.1098/rspa.2017.0649
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
In arid or semi-arid ecosystems, water availability is one of the primary controls on vegetation growth. When subsurface water resources are unavailable, the vegetation growth is dictated by the rainfall, and the random nature of the rainfall arrivals and quantities induces a probability distribution of soil moisture and vegetation biomass via the coupled dynamic equations of biomass balance and water balance. We have previously obtained an exact solution for these distributions under certain conditions, and shown that the mapping of rainfall variability to observed biomass variability can be successfully applied to a field site. Here, we expand upon our earlier theoretical work to show how the dynamics can give rise to more complicated, bimodal (and multimodal) structures in the biomass distribution when positive feedbacks between growth and water availability are included. We also derive some new analytical results for the crossing properties of this system, which enable us to determine on what time scale the effects of these feedbacks will be felt, and, relatedly, how long the system will take to cross between different modes.
引用
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页数:21
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