Two-year oscillation of monsoon rainfall and global climate in the present decade Debasis Sengupta,...

Two-year oscillation of monsoon rainfall and global climate in the present decade

Debasis Sengupta, Arathy Menon

CAOS, Indian Institute of Science, Bangalore

Data

TRMM 3B42 V6 daily 0.25⁰ rainfall 1998-2006

TRMM TMI daily 0.25⁰ SST 1998-2006

QuikSCAT/FSU daily 0.5 ⁰ wind 1999-2005

CPC monthly 0.5 ⁰ air temperature 1998-2006

TBO in Rainfall

Central India-Bay of Bengal (CI-BoB)

Wet: 1999, 2001, 2003, 2005

Dry: 2000, 2002, 2004

Are the recent biennial oscillations significant?

D(i)= R(i+1) – R(i) MD=1/N ∑ |D(i)|

TBO in SST

East Pacific SST does not have biennial oscillation.

Pacific SST: El Nino years with Indian monsoon drought minus El Ninoyears without drought (Krishnakumar et al., 2006, Science)

Central Pacific SST (“El Nino Modoki” Ashok et al., 2007); Trans Nino Index (Krishnakumar et al., 2006) do not have significant biennial oscillation.

SOI does, but only in 2001-2006

Arctic Oscillation

Thompson and Wallace (1998) GRL

http://www.jisao.washington.edu/wallace/

Northward shift of Atlantic ITCZ

Atlantic ITCZ shifted north

ITCZ shift towards warmer hemisphere Kushnir et al. (2006) J. Clim.Broccoli et al. (2006) GRLWang et al., Chiang and Koutavas (2004) Nature

AMO: Warm North Atlantic, stronger Asian monsoon Goswami et al. (2006) GRLZhang and Delworth (2006) GRL

Atlantic Meridional Mode (AMM)

No previous report of biennial Variability in AMM

From Kushnir et al., 2006

Tropical N. Atlantic winter SST: Evaporation changes in autumn (~10-15 W/m2). Insolation changes are ~3-5 W/m2.

ConclusionsModern observations show clear two-year oscillation in CI-BoB

and far West Pacific summer monsoon rain in 1999- 2005.2002 is a weak ENSO year, but East Pacific SST does not have a

two-year oscillation. Biennial oscillation (TBO) of monsoon is part of pervasive TBO

of global surface climate, including west Indian, west Pacific and tropical north Atlantic SST; the Arctic Oscillation; north Asia and north America surface air temperature.

Summer ITCZ over Bay of Bengal/India is intensified in the north. Atlantic and central Pacific winter ITCZ shifts north by ~2⁰ in years of warm northern hemisphere (tropical north Atlantic, north Eurasia and north America).

Models suggest that biennial variance of tropical climate increases as the earth warms (Nanjundiah et al. 2005 ASL) – are we seeing the first signs ?

TBO in Wind speed