Table 2 Descriptions of parameters in the vertically resolved model

From: Model structures amplify uncertainty in predicted soil carbon responses to climate change

Short name

Description

Unit

LL

UL

Default

Mean ± SD

G-R

D 1

Diffusivity in non-permafrost regions

m2 yr−1

0.3 × 10−4

16 × 10−4

1 × 10−4

(1.4 ± 0.81) × 10−4

1.02

D 2

Diffusivity in permafrost regions

m2 yr−1

0.3 × 10−4

16 × 10−4

4 × 10−4

(9.3 ± 4.0) × 10−4

1.00

z t

e-folding depth for depth scalar

m

0

1

0.5

0.41 ± 0.05

1.00

t 1

Coefficient to calculate f21 (intercept)

–

0

1

0.85

0.28 ± 0.14

1.00

t 2

Coefficient to calculate f21 (slope)

–

0

1

0.68

0.089 ± 0.069

1.00

f 31

Fraction of C in fast soil C transferring to passive soil C

–

0

0.01

0.005

0.0053 ± 0.0026

1.00

f 12

Fraction of C in slow soil C transferring to fast soil C

–

0.1

0.6

0.4185

0.37 ± 0.13

1.00

f 32

Fraction of C in slow soil C transferring to passive soil C

–

0

0.05

0.0315

0.031 ± 0.011

1.00

f 13

Fraction of C in passive soil C transferring to fast soil C

–

0.3

0.7

0.45

0.50 ± 0.11

1.00

k 1

Turnover rate of C from fast soil C

g C g C−1 yr−1

1

15

7.3

7.52 ± 3.76

1.00

k 2

Turnover rate of C from slow soil C

g C g C−1 yr−1

0.1

0.5

0.2

0.22 ± 0.086

1.01

k 3

Turnover rate of C from passive soil C

g C g C−1 yr−1

0.001

0.01

0.0045

0.0048 ± 0.0018

1.01

Q 10

Temperature sensitivity

–

1

3

2

1.03 ± 0.024

1.00

  1. LL lower limit, UL upper limit
  2. Parameter names, ranges, units, default values, posterior mean, and standard deviation (SD), and G-R statistics in the vertically resolved model