2. Interannual variability of the Asian summer monsoon JJA - - PowerPoint PPT Presentation

2 interannual variability of the asian summer monsoon
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2. Interannual variability of the Asian summer monsoon JJA - - PowerPoint PPT Presentation

2. Interannual variability of the Asian summer monsoon JJA precipitation (u, v) & (z-750 m) at 925 mb, July Seasonal phase lock of El Nino El Nino PostEl Nino summer summer EOFs of JJAS rainfall variability over India for 19002008.


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SLIDE 1

JJA precipitation (u, v) & (z-750 m) at 925 mb, July

  • 2. Interannual variability of the Asian summer monsoon
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SLIDE 2

Seasonal phase lock of El Nino

El Nino summer Post‐El Nino summer

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SLIDE 3

EOFs of JJAS rainfall variability over India for 1900‐2008. El Nino summer

r [PC, SOI]=0.52

Post‐El Nino summer

r [PC, Nino3.4]=‐0.xx SST Mishra et al. (2012, PNAS)

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SLIDE 4
  • Corr. w/ antecedent NDJ

Nino3.4 SST: gauge rainfall & moisture transport, w/ topography

  • Strong monthly variations.
  • Migrating anomaly bands.
  • Orographic effect.

(1979‐2014)

Post‐El Nino effect

Kaiming Hu et al. (2017, JC)

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SLIDE 5

JJA Precip EOF over Indo‐WP

Rainfall EOF PC1 PC2 JJA Nino 3.4 0.84 NDJ(‐1) Nino 3.4 0.69 JJA NIO 0.84

Concurrent El Nino Antecedent El Nino

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SLIDE 6

+

  • ENSO

IO Capacitor Indian Ocean warming persists through JJA(1), and could exert climatic influences after El Nino has dissipated. But how?

Nino NIO

NW Pac

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SLIDE 7

Correlation with preceding ENSO (NDJ): Tropospheric temp, surface wind & rainfall

IO warming  Warm Kelvin wave into the WP  Northeasterly winds to the north under friction  Divergence over NW Pacific  Suppressed convection Indian Ocean Capacitor Effect

Post‐El Nino summer

Xie et al. (2009, JC)

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SLIDE 8

Hamouda & Kucharski (2018, Clim Dyn)

Precip response of moist AGCM to an isolated SST

perturbation w/ NS symmetric mean SST

Ekman divergence suppresses convection off equator to the east.

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SLIDE 9

IO Warming  NW Pacific anticyclone  Easterly anomalies Reduced SW monsoon

Coupled Indo-western Pacific ocean capacitor (IPOC) Coupled Indo-western Pacific ocean capacitor (IPOC)

Post‐El Nino summer

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SLIDE 10

Concurrent El Nino Antecedent El Nino

Summary

  • ENSO affects the Asian summer monsoon in both

concurrent and subsequent summers.

  • Indo‐western Pacific ocean capacitor (IPOC) gives rise

to post‐ENSO summer anomalies.

Xie, S.-P. et al., 2016: Indo-western Pacific ocean capacitor and coherent climate anomalies in post-ENSO summer: A review. Adv. Atmos. Sci., 33, 411-432.