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Regime shifts by front dynamics

机译:政权由前动力转变

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摘要

Ecosystems are highly nonlinear dissipative systems that often admit multiple alternative stable states, but seldom have the time span to converge to these states as they are repeatedly interfered by environmental changes and disturbances. Multiplicity of stable states in variable and disturbed environments is of high concern because of the possible occurrence of regime shifts, i.e. state transitions that involve large, abrupt decline in ecosystem function. State transitions induced by disturbances, however, need not be abrupt as the disturbances are often limited in their spatial extent. In that case they induce local state transitions that result in spatially confined alternative-state domains. The subsequent dynamics crucially depend on the dynamics of the transition zones or fronts that bound these domains. In this paper we study three aspects of front dynamics that affect the nature of regime shifts and their outcomes: single-front motion, front interactions and front instabilities. Using models of dryland vegetation as a case study we show that fronts can change their speed and invert their direction of motion as parameters change across a threshold value – the Maxwell point, that fronts may slow down or stop entirely when interacting with other fronts, and that disturbances may change one front type to another, each with its distinct speed. We further study the implications of these three aspects of front dynamics to gradual regime shifts. We show that such shifts can occur due to the propagation of a perturbation beyond its original extent, that such a transition does not necessarily culminate in the alternative state, i.e. it may remain incomplete, and that the time it takes for a regime shift to occur can be changed by front manipulations. Since gradual regime shifts can take place far from the typical tipping point considered, early warning signals of an approaching tipping point would fail in predicting gradual regime shifts. A more relevant approach for these regime shifts may be the development of detection and prevention methods, which can be applied during an ongoing gradual regime shift due to its slow dynamics. We conclude with a discussion of the need to develop such methods and of other ecological contexts that may benefit from them.
机译:生态系统是高度非线性的耗散系统,通常会允许多个替代稳定状态,但是很少有时间收敛到这些状态,因为它们反复受到环境变化和干扰的干扰。由于可能发生政权转移,即涉及生态系统功能突然大幅度下降的状态转换,因此在可变和受干扰的环境中的多个稳定状态备受关注。然而,由于扰动通常在其空间范围上受到限制,因此不需要突然扰动状态转换。在那种情况下,它们会引起局部状态转换,从而导致空间受限的替代状态域。后续动力学至关重要地取决于限制这些区域的过渡带或前沿的动力学。在本文中,我们研究了影响政权变动性质及其结果的前部动力学的三个方面:单前部运动,前部相互作用和前部不稳定。使用旱地植被模型作为案例研究,我们发现,当参数在阈值(麦克斯韦点)上变化时,前沿可以改变速度并反转运动方向;与其他前沿互动时,前沿可能会减慢或完全停止,并且干扰可能将一种前沿类型改变为另一种,每种都有其独特的速度。我们进一步研究了前动态这三个方面对政权逐渐转移的影响。我们表明,这种转变可能是由于扰动的传播超出其原始范围而发生的,这种转变不一定以替代状态达到顶点,即它可能保持不完整,并且发生政权转变需要花费时间可以通过前面的操作进行更改。由于逐渐的政权转移可能发生在远离所考虑的典型临界点的位置,因此接近临界点的早期预警信号将无法预测逐渐的政权转移。与这些状态转换更相关的方法可能是开发检测和预防方法,由于其动态缓慢,可以在正在进行的逐渐的状态转换期间应用。最后,我们讨论了开发此类方法的必要性以及可能从中受益的其他生态环境。

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