Projected changes in potential evaporation for catchments of the Mekong Basin. 30

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3.6.1. Projected changes in basin-wide potential evaporation

Consistent with the trend in projected temperature, potential evaporation is projected to increase by 2030 in all months and all catchments. The projected increase in annual

potential evaporation averaged across the basin ranges from 1.451 m to 1.48 m, a change of 2%. Projected increases in monthly potential evaporation are 0.003 m from February to June, and 0.002 for the remaining months (Figure 3.13)

Mekong Basin

0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range GCM median potential evaporation Baseline potential evaporation

Figure 3.13. Baseline (1951-2000) versus future (2030) monthly potential evaporation.

3.6.2. Projected changes in potential evaporation for Mekong catchments The projected increase in annual potential evaporation is greatest for the Upper Mekong (0.043 m), an increase of 6% (Figure 3.14). Projected increases in annual potential

evaporation are less than 2.1% for all the remaining catchments of the basin (Figures 3.14 to 3.16). The range in projected potential evaporation is low for all months and for all

catchments, being 0.002 m or less for all months in all catchments except the Upper Mekong where the range in projected potential evaporation is 0.003 m for May.

Upper Mekong

0.00 0.05 0.10 0.15

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Chiang Saen

0.05 0.10 0.15 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Figure 3.14. Baseline (1951-2000) versus future (2030) monthly potential evaporation for catchments of the Upper Mekong basin: Upper Mekong and Chiang Saen.

Moung Nouy

0.05 0.10 0.15 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Luang Prabang

0.05 0.10 0.15 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Ventiane

0.05 0.10 0.15 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Tha Ngon

0.05 0.10 0.15 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Nakhon Phanom

0.10 0.12 0.14 0.16 0.18 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Mukdahan

0.10 0.12 0.14 0.16 0.18 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Ban Keng Done

0.08 0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Yasothon

0.10 0.12 0.14 0.16 0.18 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Figure 3.15. Baseline (1951-2000) versus future (2030) monthly potential evaporation Moung Nouy, Luang Prabang, Vientiane, Tha Ngon, Nakhon Phanom, Mukdahan, Ban Keng Done and Yasothon catchments.

Ubon Ratchathani

0.10 0.12 0.14 0.16 0.18 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Pakse

0.10 0.12 0.14 0.16 0.18 0.20

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Se San

0.08 0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Kratie

0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Tonle Sap

0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Phnom Penh

0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Border

0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Delta

0.10 0.12 0.14 0.16 0.18

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

potential evaporation (m)

GCM potential evaporation range Baseline potential evaporation GCM median potential evaporation

Figure 3.16. Baseline (1951-2000) versus future (2030) monthly potential evaporation for Ubon Ratchathani, Pakse, Se San, Kratie, Tonle Sap, Phnom Penh, Border and Delta catchments.

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