Ecoinformatics and Soil-Plant Formations - New Ecoinformatics Tools in Environmental Science: Applications and Decision-making - page 697

Table 8.11 Model evaluations of the variations in the carbon reserve when forests of northern
regions (up to 42 ° N) are burned
Years after
in

Deviation in the carbon
reserve (Gt)

Years after
in

Deviation in the carbon
reserve (Gt) fl uence fl uence

ʔ C A ʔ C S ʔ C U ʔ C AL ʔ C A ʔ C S ʔ C U ʔ C AL

0 238.1 − 7.9 24.9 0.1 60 44.2 − 49.1 14.3 20.7

10 174.2 − 31.6 47.9 4.9 70 33.1 − 41.6 10.3 21.9

− 67.6 − 35.0

20 138.9 39.2 10.0 80 20.7 7.5 22.8

30 107.9 − 90.3 32.2 13.8 90 12.9 − 30.1 5.5 23.3

40 82.0 − 64.3 24.1 16.8 100 7.3 − 24.7 3.7 23.6

50 60.9 − 56.9 18.4 19.1 200 − 12.7 − 5.9 − 1.7 21.7

Table 8.12 Model evaluations of the variations in the carbon reserve when forests of tropical
regions are burned
Years after
influence

Deviation in the carbon
reserve (Gt)

Years after
influence

Deviation in the carbon
reserve (Gt)

ʔ C A ʔ C S ʔ C U ʔ C AL ʔ C A ʔ C S ʔ C U ʔ C AL

0 406.2 − 20.0 42.2 0.2 60 2.9 − 12.4 3.0 22.8

10 264.4 − 93.7 74.1 8.0 70 − 5.8 − 7.5 0.5 22.8

20 162.2 − 84.8 48.0 14.9 80 − 11.6 − 4.2 − 0.9 22.6

30 90.6 − 38.6 27.9 19.1 90 − 13.2 − 2.6 − 1.7 22.5

40 45.4 − 36.5 15.0 21.3 100 − 14.5 − 1.9 − 2.1 21.8

50 18.3 − 21.6 7.5 22.4 200 − 13.2 − 2.3 − 1.9 17.7

Fig. 8.20 Prognoses of the
changes in average global
temperature evaluated by
means of the Hadley Centre
climate model and GMNSS in
framework of two scenarios
of energy use