1. Global monsoon features Australian monsoon South American monsoon North American monsoon African monsoon Asian monsoon 2. Northern China winter drought.

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Presentation transcript:

1. Global monsoon features Australian monsoon South American monsoon North American monsoon African monsoon Asian monsoon 2. Northern China winter drought 3. Weak Indian summer monsoon Worldwide Monsoons in

1. Global Monsoon Features (Oct 2008 – Sept 2009) JJA OLR Anomalies JJA 200-mb Vel Pot Anomalies

Australian Monsoon (Winter ) Link to La Nina condition, strong, apparent ISO

Apparent Intraseasonal Variability

The monsoon was weak during the onset phase of rainy season over southern Amazon and central-southeastern Brazil, with large rainfall deficits (>150 mm) in many areas. South American Monsoon Onset Phase (Sept-Nov 2008)

Rainfall was below average over central-southern Brazil and most of Argentina but above average over the northern Amazon Basin, features consistent with the La Niña conditions in the tropical Pacific. Mature Phase (Dec Feb 2009)

Much above-average rainfall was observed over northeastern Brazil, consistent with the La Niña conditions in the tropical Pacific and the Atlantic SST dipole pattern, contributing to an intensification and southward displacement of the Atlantic ITCZ. Another factor contributing to the rainfall anomalies in Northeast Brazil was the active MJO. Decay Phase (Mar-May 2009)

North American Monsoon (Summer 2009) Weak monsoon, in spite of an early onset Driest Months: Aug in SW U.S. Jul & Aug in Mexico Wettest Month: September

From Art Douglas Mexican National Rainfall

NAME Forecast Forum 2009 CFS T382 Clim

Weak relationship with ENSO El Nino La Nina Neutral

African Summer Monsoon (Jul-Sept 2009) Above-normal monsoon rainfall over W Sahel The rainfall over Sahel was consistent with the upward tendency of the past years.

Asian Summer Monsoon Weak monsoon over India Weak large-scale monsoon circulation Philippines constantly received above-normal monsoon rainfall. W-Y monsoon index JJA P Anom

Weak Large-scale Asian Summer Monsoon Circulation in Years (Webster-Yang Index)

2. Winter Drought in N. China Strong winter monsoon Henan Province  No precipitation over Beijing for 111 days since October 2008  Most serious in 5 decades in some locations  Disastrous damage to China’s main areas for crops  10 million hectares of crops affected, and more than 4 million people short of drinking water Clim 2008/09 Beijing Reference: Gao and Yang (2009, JGR)

Drought Categories (Oct 2008 – Jan 2009) Severe drought mainly in Dec 2008 & Jan 2009 weak moderate severe extreme Oct Jan Dec Nov

Relationship with Pacific SST La Nina condition SST anomalies in Dec- Jan Dec-Jan correlation: core drought domain and grid- point SST

Relationship with the Tibetan Plateau Less snow; warming Anomalies of 700-mb winds and T ( mb) in Dec- Jan A Opposite condition of Tibetan Plateau and snow storms affecting China in Jan 2008 (Wen et al. 2009; MWR)

3. Weak Indian Summer Monsoon 77% of JJAS normal, worst in the northwest Monsoon appeared early (23 May), but propagated northwestward too slowly during 8-20 June. From IMD O. P. Singh: Worst since th worst in record (since 1871): 67% in 1877, 71% in 1899, 75% in 1918, & 76% in 1972

Worst in June: 53% of Normal July (96%); August (73%); Sept (79%) From IMD

ENSO: Weak Indian summer monsoon after La Nina winter and before El Nino winter (Nino3.4 SST anomalies: -1.4 in DJF and +0.8 in DJF ; 0.7 in JJA 2009) Biennial feature: Weak Indian summer monsoon after strong Australian winter monsoon (strong Australian monsoon in DJF ) Subtropical-extratropical influence: Strong upper tropospheric westerlies unfavorable for strong monsoon (Webster and Yang 1992) MJO? Indian Ocean SST? And others? Over Predicted! Causes of the weak monsoon? DJF JJA

1. Global monsoon features Strong Australian monsoon Weak South American monsoon (delayed onset) Weak North American summer monsoon (early onset) Strong African summer monsoon (long-term change) Weak Asian summer monsoon (apparent regional features) 2. Northern China winter drought Influences of ENSO, Tibetan Plateau, … 3. Weak Indian summer monsoon ENSO impact, biennial feature, subtropical-extratropical influence, … Summary