scholarly journals Adaptive self-organization of Bali’s ancient rice terraces

2017 ◽  
Vol 114 (25) ◽  
pp. 6504-6509 ◽  
Author(s):  
J. Stephen Lansing ◽  
Stefan Thurner ◽  
Ning Ning Chung ◽  
Aurélie Coudurier-Curveur ◽  
Çağil Karakaş ◽  
...  

Spatial patterning often occurs in ecosystems as a result of a self-organizing process caused by feedback between organisms and the physical environment. Here, we show that the spatial patterns observable in centuries-old Balinese rice terraces are also created by feedback between farmers’ decisions and the ecology of the paddies, which triggers a transition from local to global-scale control of water shortages and rice pests. We propose an evolutionary game, based on local farmers’ decisions that predicts specific power laws in spatial patterning that are also seen in a multispectral image analysis of Balinese rice terraces. The model shows how feedbacks between human decisions and ecosystem processes can evolve toward an optimal state in which total harvests are maximized and the system approaches Pareto optimality. It helps explain how multiscale cooperation from the community to the watershed scale could persist for centuries, and why the disruption of this self-organizing system by the Green Revolution caused chaos in irrigation and devastating losses from pests. The model shows that adaptation in a coupled human–natural system can trigger self-organized criticality (SOC). In previous exogenously driven SOC models, adaptation plays no role, and no optimization occurs. In contrast, adaptive SOC is a self-organizing process where local adaptations drive the system toward local and global optima.

2019 ◽  
Vol 234 ◽  
pp. 767-778 ◽  
Author(s):  
Jiewu Leng ◽  
Pingyu Jiang ◽  
Kailin Xu ◽  
Qiang Liu ◽  
J. Leon Zhao ◽  
...  

2014 ◽  
Vol 44 (5) ◽  
pp. 1285-1305 ◽  
Author(s):  
T. Radko ◽  
J. D. Flanagan ◽  
S. Stellmach ◽  
M.-L. Timmermans

Abstract This study explores the dynamics of thermohaline staircases: well-defined stepped structures in temperature and salinity profiles, commonly observed in regions of active double diffusion. The evolution of staircases in time is frequently characterized by spontaneous layer-merging events. These phenomena, the authors argue, are essential in regulating the equilibrium layer thickness in fully developed staircases. The pattern and mechanics of merging events are explained using a combination of analytical considerations, direct numerical simulations, and data analysis. The theoretical merger model is based on the stability analysis for a series of identical steps and pertains to both forms of double diffusion: diffusive convection and salt fingering. The conceptual significance of the proposed model lies in its ability to describe merging events without assuming from the outset specific power laws for the vertical transport of heat and salt—the approach adopted by earlier merging models. The analysis of direct numerical simulations indicates that merging models based on the four-thirds flux laws offer adequate qualitative description of the evolutionary patterns but are less accurate than models that do not rely on such laws. Specific examples considered in this paper include the evolution of layers in the diffusive staircase in the Beaufort Gyre of the Arctic Ocean.


1982 ◽  
Vol 44 (2) ◽  
pp. 135-140 ◽  
Author(s):  
Teuvo Kohonen

1987 ◽  
Vol 10 (2) ◽  
pp. 183-183 ◽  
Author(s):  
Gerhard Werner

2013 ◽  
Vol 20 (9) ◽  
pp. 092306 ◽  
Author(s):  
Andrew P. L. Newton ◽  
Eun-jin Kim ◽  
Han-Li Liu

2017 ◽  
Vol 24 (1) ◽  
pp. 777 ◽  
Author(s):  
William San Martín

Abstract The widespread use of nitrogen (N) fertilizers during the second half of the 20th century radically transformed agricultural production and ecosystems on a global scale. Although the "N challenge" or the "N problem" has had limited public attention compared to biodiversity loss and climate change, scientists consider N pollution a leading ecological concern for the 21st century. Accordingly, a major challenge for scientists and policymakers around the world today is how to meet food production demands while also protecting the environment. Using Chile as a case study—one of the highest consumers of N fertilizer per hectare in the Americas—this article examines the transnational politics of production and destruction in this process of agricultural modernization. In the Cold War context, a transnational network of scientists, agencies, and authorities created an institutional framework for the transference of knowledge and technology in Chile during the 1960s. Paradoxically, as local and global reliance on N fertilizers increased, scientists were able to generate a narrative about the negative environmental effects of intensive N use and highlight the ecological limits of the Green Revolution. After 1973, however, this knowledge network suffered as a result of the Chilean government's anti-communist crackdown and adoption of market-based agricultural policies. Understanding this history of how politics shaped N consumption, science, and policy is critical to current efforts to create new of agricultural production on a regional and global scale. Keywords: nitrogen, fertilizers, the Green Revolution, Cold War, Chile, science, environment, policy, Global Nitrogen Challenge, agriculture, United States


Geophysics ◽  
2007 ◽  
Vol 72 (1) ◽  
pp. I1-I11 ◽  
Author(s):  
Maurizio Fedi

We show that potential fields enjoy valuable properties when they are scaled by specific power laws of the altitude. We describe the theory for the gravity field, the magnetic field, and their derivatives of any order and propose a method, called here Depth from Extreme Points (DEXP), to interpret any potential field. The DEXP method allows estimates of source depths, density, and structural index from the extreme points of a 3D field scaled according to specific power laws of the altitude. Depths to sources are obtained from the position of the extreme points of the scaled field, and the excess mass (or dipole moment) is obtained from the scaled field values. Although the scaling laws are theoretically derived for sources such as poles, dipoles, lines of poles, and lines of dipoles, we give also criteria to estimate the correct scaling law directly from the data. The scaling exponent of such laws is shown to be related to the structural index involved in Euler Deconvolution theory. The method is fast and stable because it takes advantage of the regular behavior of potential field data versus the altitude [Formula: see text]. As a result of stability, the DEXP method may be applied to anomalies with rather low SNRs. Also stable are DEXP applications to vertical and horizontal derivatives of a Newtonian potential of various orders in which we use theoretically determined scaling functions for each order of a derivative. This helps to reduce mutual interference effects and to obtain meaningful representations of the distribution of sources versus depth, with no prefiltering. The DEXP method does not require that magnetic anomalies to be reduced to the pole, and meaningful results are obtained by processing its analytical signal. Application to different cases of either synthetic or real data shows its applicability to any type of potential field investigation, including geological, petroleum, mining, archeological, and environmental studies.


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