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Table 1 The values of parameter setting of the RRI model used in the study

From: Assessing the effects of climate change on flood inundation in the lower Mekong Basin using high-resolution AGCM outputs

Parameters

Mountains

Plains

Manning’s coefficient for slope

n

(m−1/3s)

0.4

0.015

Soil depth

d

(m)

2.0

Lateral saturated hydraulic conductivity

ka

(m/s)

0.1

Parameter of unsaturated hydraulic conductivity

β

9.0

Vertical hydraulic conductivity

kv

(cm/h)

0.06

Soil porosity

φ

0.6

Wetting front soil suction head

Sf

0.273

Manning’s coefficient for river

nriver

(m−1/3s)

0.03