Table 2 The optimal embedding dimensions (E) and degree of nonlinearity (θ) of time-series observations.

From: Detecting causal relationship of non-floodplain wetland hydrologic connectivity using convergent cross mapping

Attributes

E

Nonlinearity

NFW

3

θ = 3.0, E = 4

GW

2

θ = 4.0, E = 3

DWorg

3

θ = 0.75, E = 3

DWadj

2

θ = 8, E = 10

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