Top Banner
Past and future European climate trends: uncertainty due to internal variability L. Terray and C. Deser CERFACS/CNRS & NCAR/CGD/CAS.
16

Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Apr 15, 2017

Download

Self Improvement

Ingrid LE RU
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Past and future European climate trends: uncertainty due to internal

variability

L. Terray and C. Deser CERFACS/CNRS & NCAR/CGD/CAS.

Page 2: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Observed temperature trends: 1963-2012

°C

DJF JJA

DJF

JJA

°C / 50 years

Page 3: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Thermodynamical Dynamical

Forced ? ?

Free ? ?

A paradigm for surface air temperature (SAT) change

Page 4: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

All possible trends … Observations ???

°C / 50 years

Page 5: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Range from 0 to 3°C in 50 years

°C / 50 years

Page 6: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Total trends

0 °C / 50 years 2.5 °C / 50 years

°C / 50 years

Member 12 Member 7

Page 7: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Dynamical component using SLP analogues

-0.56 °C / 50 years 1.1 °C / 50 years

°C / 50 years

Member 12 Member 7

°C / 50 years

Page 8: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Thermodynamical component

0.56 °C / 50 years 1.4 °C / 50 years

Member 12 Member 7

°C / 50 years

Page 9: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Thermodynamical component driver ?

°C

EOF1

45%

EOF2

14%

Snow frac.

%

Snow frac.

Page 10: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Dynamical adjustment and time of emergence

Total SAT Dynamically-adjusted

Page 11: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Dynamical adjustment and seasonal differences

Winter Summer

1963-2012 trend (°C / 50 years):

Raw SAT: 2.5 2.

Adjusted: 1.8 1.8

Member 12

Page 12: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Observations: SAT decomposition

°C / 50 years

Page 13: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Western Europe is warming (1.8 K / 50 years in winter) Analysis of CESM1 LE suggests a possible large contribution

from internal variability (same magnitude as the forced response)

Main contribution comes from the dynamical component Dynamical adjustment increases signal to noise ratio (more

in winter than summer) and advances time of emergence Spread in internal thermodynamical component related to

the ocean state and land-atmosphere interactions (snow effect dominant in winter)

No discrepancy between CESM1 and observations Dynamically adjusting observations suggests that half of

the observed trend could be due to unpredictable decadal changes in atmospheric circulation

Summary

Page 14: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Winter SAT 1963-2012 trends

1.2 °C / 50 years 1.8 °C / 50 years

CESM1 Ens.Mean Obs

°C / 50 years

Page 15: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Member 12: free and forced components

1.3 °C/50yr 1.2 °C/50yr

2.5 °C/50yr

Total

Free Forced

Page 16: Terray l 20150708_1500_upmc_jussieu_-_room_101_(building_14-24)

Dynamical and thermodynamical free components

0.9 °C / 50 years 0.4 °C / 50 years

Dynamical Thermodynamical