DOAJ Open Access 2021

Mid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble

E. Berntell Q. Zhang Q. Li A. M. Haywood J. C. Tindall +32 lainnya

Abstrak

<p>The mid-Pliocene warm period (mPWP; <span class="inline-formula">∼3.2</span> million years ago) is seen as the most recent time period characterized by a warm climate state, with similar to modern geography and <span class="inline-formula">∼400</span> ppmv atmospheric CO<span class="inline-formula"><sub>2</sub></span> concentration, and is therefore often considered an interesting analogue for near-future climate projections. Paleoenvironmental reconstructions indicate higher surface temperatures, decreasing tropical deserts, and a more humid climate in West Africa characterized by a strengthened West African Monsoon (WAM). Using model results from the second phase of the Pliocene Modelling Intercomparison Project (PlioMIP2) ensemble, we analyse changes of the WAM rainfall during the mPWP by comparing them with the control simulations for the pre-industrial period. The ensemble shows a robust increase in the summer rainfall over West Africa and the Sahara region, with an average increase of 2.5 mm/d, contrasted by a rainfall decrease over the equatorial Atlantic. An anomalous warming of the Sahara and deepening of the Saharan Heat Low, seen in <span class="inline-formula"><i>&gt;</i>90</span> % of the models, leads to a strengthening of the WAM and an increased monsoonal flow into the continent. A similar warming of the Sahara is seen in future projections using both phase 3 and 5 of the Coupled Model Intercomparison Project (CMIP3 and CMIP5). Though previous studies of future projections indicate a west–east drying–wetting contrast over the Sahel, PlioMIP2 simulations indicate a uniform rainfall increase in that region in warm climates characterized by increasing greenhouse gas forcing. We note that this effect will further depend on the long-term response of the vegetation to the CO<span class="inline-formula"><sub>2</sub></span> forcing.</p>

Penulis (37)

E

E. Berntell

Q

Q. Zhang

Q

Q. Li

A

A. M. Haywood

J

J. C. Tindall

S

S. J. Hunter

Z

Z. Zhang

Z

Z. Zhang

X

X. Li

C

C. Guo

K

K. H. Nisancioglu

K

K. H. Nisancioglu

C

C. Stepanek

G

G. Lohmann

G

G. Lohmann

L

L. E. Sohl

L

L. E. Sohl

M

M. A. Chandler

M

M. A. Chandler

N

N. Tan

N

N. Tan

C

C. Contoux

G

G. Ramstein

M

M. L. J. Baatsen

A

A. S. von der Heydt

A

A. S. von der Heydt

D

D. Chandan

W

W. R. Peltier

A

A. Abe-Ouchi

W

W.-L. Chan

Y

Y. Kamae

C

C. J. R. Williams

C

C. J. R. Williams

D

D. J. Lunt

R

R. Feng

B

B. L. Otto-Bliesner

E

E. C. Brady

Format Sitasi

Berntell, E., Zhang, Q., Li, Q., Haywood, A.M., Tindall, J.C., Hunter, S.J. et al. (2021). Mid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble. https://doi.org/10.5194/cp-17-1777-2021

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Informasi Jurnal
Tahun Terbit
2021
Sumber Database
DOAJ
DOI
10.5194/cp-17-1777-2021
Akses
Open Access ✓