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Page 1: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only
Page 2: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

The South Pacific Blob and the Pressure Trend Dipole

Expect the unexpected

With René Garreaud1, Kyle Clem2 and José Vicencio3

Thanks also to Roberto “Rossby” Rondanelli,

Juan Pablo “trendy” Boisier and Mark “believer” Falvey

Now playing at Universidad de Chile (21-01-2020)

PG32

(1) DGF-UCh + CR2 (2) VUW NZ, (3) DMC

Page 3: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

The South Pacific Blob and the Pressure Trend Dipole

• Background: Their motivation, our motivation • Pressure Trend: Revisit and update • The Southern Blob • Attribution • Conclusions

Page 4: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

1979-2013

Huston….we have a problem! CMIP5 trends oppose their observational counterparts around Antarctic

Page 5: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Long term mean SLP (ERA5)

Page 6: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

R. Fogt, 2018. Based on ERA-SLP

Page 7: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Causes of the ABS low deepening?

Page 8: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Nature is complicated and observation-only analysis can be confused when multiple forcing are playing at the

same time. A little help from models!

Atmosphere

Prescribed SST & SIC

Constant, Prescribed Radiative forcing

Atmosphere

Ocean Ocean

Varying Radiative forcing

Prescribed SST & SIC

AMIP models Ensemble mean reveals the atmospheric

response forced by prescribed SST anomalies

Fully coupled models Ensemble mean reveals the ocean/atmos

response forced by a prescribed change in RF

Page 9: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

SST trend 1979-2012

CAM4 SLP Response

Tropical forcing of high latitude circulation

Page 10: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Observed trends

CAM3 Central Pacific drying

forced response

IPO transition from warm to cold CPac drying ABS low deepening Changes in Antarctic SIC

Page 11: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Large-scale context for central Chile droughts

ABS low and SEP anticyclone play a key role Both modulated by ENSO

Page 12: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

The 2010-2018 mega drought in Central Chile Mostly ENSO neutral!

Page 13: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only
Page 14: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

PDO (IPO) index until 2014 (Tokyo climate center)

Ok for long-term drying and first half of mega drought, but….

Page 15: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

PDO (IPO) index until now (Tokyo climate center)

….Not enough for 2015 onwards

Page 16: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

ERA20C

ERA-Int

NNR

ER-SST

HadISST

OI SST

Win

ter SST @ SSW

P

30

-40°S 1

90

-21

0°W

Win

ter

SLP

@ A

BS

70

-60

°S 1

30

-90°

W

What (else) is sustaining the ABS low deepening / mega drought until now?

Page 17: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

(a) SLP

(b) Z500

(c) SST

(d) Precip

hPa/dec

gpm/dec

°C/dec

mm/day/dec

Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5)

+0.6

-1.0

Page 18: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Win

tert

ime

(MJJ

AS)

40

yea

r tr

end

s (1

97

9-

20

18

) fr

om

sel

ecte

d f

ield

s (E

RA

5)

Page 19: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

(a) SLP Congruent with CPAC

(b) SLP Congruent with SAM

(c) Residual (Full - CPAC + SAM)

hPa decade-1

+0.6

-1.0

+0.6

-1.0

+0.6

-1.0

Linear congruency analysis:

Y = aF + b dY = aF

Page 20: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

(a) SLP Congruent with CPAC

(b) SLP Congruent with SAM

(c) Residual (Full - CPAC + SAM)

hPa decade-1

+0.6

-1.0

+0.6

-1.0

+0.6

-1.0

Linear congruency analysis:

Y = aF + b dY = aF

Both CPac (IPO) and SAM (CC) are part of the story but only accounts for about half of the observed trends

Page 21: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

J. Vicencio 2020

Page 22: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Satellite-based (altimetry minus GRACE-CSR) steric sea level trend over 2005–2014.

The Southern Blob (30-40°S, 190-210°E)

Page 23: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

The Southern Blob (30-40°S, 190-210°E)

Page 24: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

SLP (hPa) Z500 (mgp) Prec (mm/day)

Full

SST

Without

SSWP

Difference:

With –

Without

SSWP

CESM results: CLIMO+dSST minus CLIMO

Page 25: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

SLP (hPa) Z500 (mgp) Prec (mm/day)

Full

SST

Without

SSWP

(0.5%

area)

Difference:

With –

Without

SSWP

CESM results: CLIMO+dSST minus CLIMO

Page 26: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

SLP (hPa) Z500 (mgp) Prec (mm/day)

Full

SST

Without

SSWP

Difference:

With –

Without

SSWP

CESM results: CLIMO+dSST minus CLIMO

Southern Blob direct effect

Page 27: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Is the southwest subtropical Pacific causing the pressure drop over the ABS?

SLP Trend 1980 – 2015 calculated with SPEEDY

Control (Full SST) No SSWP SST

Vicencio 2020

Page 28: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

(a) SST Trend (°C/40-yr)

(b) SLP Trend (hPa/40-yr)

(c) Precipitation Trend (mm/day/40-yr)

The Southern Blob in the past? 51 Pre-industrial fully coupled simulations. Composite of largest 40-year warming periods in the SSWP

• Similar to present climate trends but amplitude is unprecedented.

• Signature of CPac (and SAM) are also present….

Page 29: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Initial CPac Forcing

Self sustaining S Southern Blob

(Warm advection + downwelling)

NE winds

NE winds

Blocked storm track

Work in progress • AtmosOcean hypotesis to be tested with OMIP experiments • SAM (CC) role • Mechanism for eastward expansion

SAM

Page 30: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only
Page 31: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only
Page 32: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

The widely publizised early summer 2020 blob grew under the same mechansism proposed here, but it was short lived because mother high was MJO-related and faded by the early January ….

Page 33: The South Pacific Blob - Universidad de Chile · Wintertime (MJJAS) 40 year trends (1979-2018) from selected fields (ERA5) +0.6 -1.0 (1979-A5) (a) SLP Congruent with CPAC ... only

Precipitation Anomalies (%) SAT Anomalies (°C)

CMIP5 Models: Present (2010-2020, RCP8.5) minus recent past (1970-2000, HIST)

Multi model mean (43 models)

Dry – Wet CCH (7 models each)

-5% 4%

SLP Anomalies (hPa)