Table 2 Percent increase of inundation metrics from current climate to 2100 for four different models. These values are calculated as follows: \(Rate\, of\, increase\, of\, X \left(\%\right)=({X}_{2100}-avg(X)/avg({X}_{2000})\).

From: A sensitivity study of rising compound coastal inundation over large flood plains in a changing climate

 

HiRAM-GFDL

RCP4.5

1 m SLR

CAM5.1

RCP8.5

1 m SLR

GFDL6-ESM4-KE

RCP4.5

1 m SLR

FSUGSM-

WRF

AMO-

RCP4.5

1 m SLR

FSUGSM-

WRF

AMO+

RCP4.5

1 m SLR

FSUGSM-

WRF

AMO+

RCP8.5

1 m SLR

FSUGSM-

WRF

AMO+

RCP8.5

2 m SLR

AIH (%)

68

79

68

88

94

134

194

MIH (%)

75

120

78

80

125

200

238

TIA (%)

46

50

44

84

107

124

158

TIV (%)

140

228

114

171

246

367

568