Effect of the 2009 MaddenJulian Oscillation on the 2010 Polar Stratosphere Lisa Neef1, Katja Matthes1, Sebastian Wahl1, Kevin Raeder2 1GEOMAR

Helmholtz Centre for Ocean Research Kiel 2National Center for Atmospheric Research

Intraseasonal Predictability with Stratospheric Teleconnections

Butler et al. 2014

Effect of the MJO on 2009/10 Winter | 28 June 2015

MJO effect on AO/NAO Stratospheric Pathway MJO Phase Frequency preceeding SSWs

Z500 Anomalies 3-5 Weeks after MJO 3

Garfinkel et al. 2012

MJO phase 3 precedes SSW by 3-5 Weeks, because this phase influences the region most strongly associated with PW1 driving. Effect of the MJO on 2009/10 Winter | 28 June 2015

Winter 2009/10 Extreme negative AO/NAO

Record cold outbreaks

Major SSW in late Jan

Wind

Temp

Jung et al. 2011

Cohen et al. 2010

Effect of the MJO on 2009/10 Winter | 28 June 2015

Ayarzaguena et al. 2014

Winter 2009/10 Extreme negative AO/NAO

Oct-Dec MJO Mostly Phase 1-3

Major SSW in late Jan

Wind

Temp

Jung et al. 2011

Effect of the MJO on 2009/10 Winter | 28 June 2015

Ayarzaguena et al. 2014

Winter 2009/10 Jung et al. 2011: Nudging different regions to reanalysis

Can’t replicate the observed PNA/NAO pattern.

Effect of the MJO on 2009/10 Winter | 28 June 2015

Constraining Tropical Variations Using Data Assimilation

DART is an Ensemble Kalman Filter that wraps around dynamical models and constrains them with data. Anderson et al. 2009 Raeder et al. 2012

DART-WACCM

Effect of the MJO on 2009/10 Winter | 28 June 2015

Constraining Tropical Variations Using Data Assimilation Obs from radiosondes, aircraft, COSMIC

40-member ensemble of WACCM 1 Oct 2009 Image: Jeff Anderson, NCAR

6-hourly updates (u,v,T,q,ps)

Effect of the MJO on 2009/10 Winter | 28 June 2015

40-member ensemble of WACCM 31 Mar 2009

Constrained WACCM Ensembles Winter 2009/10 No Assimilation + No + NoAssimilation Assimilation Observed SSTs + Observed ObservedSSTs SSTs

PDF of winter states given El Nino conditions

No Assimilation + No Assimilation + Assimilation 30S-30N Observed SSTs Observed SSTs + Observed SSTs

PDF of winter states given El Nino conditions + MJO

No Assimilation + No Assimilation + Assimilation Global Observed SSTs Observed SSTs + Observed SSTs

PDF of winter states given everything we know (like reanalysis)

Effect of the MJO on 2009/10 Winter | 28 June 2015

MJO in the Unconstrained Ensemble MJO Oct-Dec 2009

Upwelling Longwave Flux at Top of Model (W/m2)

5 Nov (MJO 2) 10 Nov (MJO 3)

19 Nov (MJO 4) 21 Dec (MJO 4)

Effect of the MJO on 2009/10 Winter | 28 June 2015

MJO in the Constrained Ensemble MJO Oct-Dec 2009

Upwelling Longwave Flux at Top of Model (W/m2)

5 Nov (MJO 2) 10 Nov (MJO 3)

19 Nov (MJO 4) 21 Dec (MJO 4)

Effect of the MJO on 2009/10 Winter | 28 June 2015

AO/NAO in the Constrained Ensemble Global DA

NOVEMBER Z500 Anomaly With respect to NoDA ensemble (which has El Nino!)

Effect of the MJO on 2009/10 Winter | 28 June 2015

Tropical DA

AO/NAO in the Constrained Ensemble Global DA

DECEMBER Z500 Anomaly With respect to NoDA ensemble (which has El Nino!)

Effect of the MJO on 2009/10 Winter | 28 June 2015

Tropical DA

AO/NAO in the Constrained Ensemble Global DA

JANUARY Z500 Anomaly With respect to NoDA ensemble (which has El Nino!)

Effect of the MJO on 2009/10 Winter | 28 June 2015

Tropical DA

AO/NAO in the Constrained Ensemble Global DA

FEBRUARY Z500 Anomaly With respect to NoDA ensemble (which has El Nino!)

Effect of the MJO on 2009/10 Winter | 28 June 2015

Tropical DA

AO/NAO in the Constrained Ensemble NoDA („El Nino Only“)

Tropical DA

Inverse Z500 polar cap

Global DA

Constraining the tropics increases probability of negative AO. Effect of the MJO on 2009/10 Winter | 28 June 2015

SSW in the Constrained Ensemble NoDA „El Nino Only“

Tropical DA

Global DA

Z 30-3hPa polar cap

Constraining the tropics increases chances of the February SSW. Effect of the MJO on 2009/10 Winter | 28 June 2015

Summary & Outlook This study

Garfinkel et al. 2012

22-33 days after MJO 3

1-20 d before SSW

Feb 2010 anomaly wrt El Nino Climatology

Effect of the MJO on 2009/10 Winter | 28 June 2015

Feb 2010 „tropical component“

Summary & Outlook Evaluating winter 2009/10 by constraining only the tropics to data using DART-WACCM.

Questions remaining… How does tropical DA constrain PW injection into the stratosphere?

Can we verify the mechanism of Garfinkel et al. (2012)?

Effect of the MJO on 2009/10 Winter | 28 June 2015

Tropical dynamics affect: AO/NAO

SSW

Effect is separate from the effect of El Nino. What about other winters?

Effect of the MJO on 2009/10 Winter | 28 June 2015

References

Effect of the MJO on 2009/10 Winter | 28 June 2015

Winter 2009/10

Wang & Chen 2010

Effect of the MJO on 2009/10 Winter | 28 June 2015

Constraining subseasonal tropical variability with data assimilation Relative Humidity from COSMIC

Assimilate this and other data into the tropics of an atmosphere model

Effect of the MJO on 2009/10 Winter | 28 June 2015

DART-WACCM Observations

Effect of the MJO on 2009/10 Winter | 28 June 2015

DART-WACCM vs. ERA-Interim COSMIC

DART-WACCM

ERA-Interim WACCM free

Effect of the MJO on 2009/10 Winter | 28 June 2015

Madden Julian Oscillation

Image by F. Martin www.climate.gov

Image by A. Matthews envam1.env.uea.ac.uk/mjo.html

Effect of the MJO on 2009/10 Winter | 28 June 2015

MJO effect on AO/NAO Short Timescale MJO phase frequency for +/AO tendency

L‘Heureux & Higgins 2008

Z500 Anomaly 40-60N following MJO phase 3

Cassou 2008

Z500 Anomaly following MJO phase 7 with 10-day lag

Lin et al. 2009

MJO phase 7 leads to a negative AO roughly 1-2 weeks later.

ENSO 2009/10

Global SST anomalies (C), NOAA (Buchan et al. 2014)

Effect of the MJO on 2009/10 Winter | 28 June 2015

MJO effect on AO/NAO Short Timescale Study

Result

MJO phase related to NAO-

Cassou 2008

MJO phases XX excite PWs that break in extratropical troposphere.

MJO 6-7 at lag 6-12 days

L‘Heureux & Higgins 2008

AO tendency proportional to MJO phase

MJO 7-8

Lin et al. 2009

MJO 6-8 (2-4) causes PW propagation to extratropical Atlantic basin, causing -(+) NAO.

MJO 6-8 at lag 5-15 days

Winter 2009/10 Study

Finding

Wang & Chen 2010

Negative AO anomaly propagated downward from the stratosphere. Late Nov SSW possibly excited by blocking over Alaska.

Jung et al. 2011

Cannot replicate negative AO by constraining sea ice, SSTs, tropics, stratosphere, solar cycle, snow cover

Ayarzaguena et al. 2011

SSW excitation due to a mix of RW and RW interaction with climatological waves.

Fereday et al. 2012

Extreme AO/NAO easier to predict with a high top model.

Effect of the MJO on 2009/10 Winter | 28 June 2015

Helmholtz-Zentrum für Ozeanforschung Kiel (Arial 45 ...

Ayarzaguena et al. 2014. Cohen et al. 2010. Jung et al. 2011. Extreme negative AO/NAO. Record cold ... Tropical DA. Global DA. NOVEMBER. Z500 Anomaly.

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