New paper finds Indian monsoons correlate with solar activity & decreased intensity with warming

In another blow to the alarmist fallacy that global warming causes more extreme weather, a paper published last week finds the intensity of the Indian summer monsoon has gradually decreased over the past 150 years. Furthermore, the authors find solar activity may be responsible for cyclical patterns in monsoon intensity.

CLIMATE DYNAMICS

2012, DOI: 10.1007/s00382-012-1378-0

Decreasing Asian summer monsoon intensity after 1860 AD in the global warming epoch

Abstract

The trend of the Indian summer monsoon (ISM) intensity and its nature during the past 100 and 200 years still remain unclear. In this study we reconstructed the ISM intensity during the past 270 years from tree ring δ¹⁸O at Hongyuan, eastern edge of the Tibet Plateau. The monsoon failures inferred from δ¹⁸O_{tree ring} correlate well with those recorded in ice cores, speleothem, and historical literature sources. 22.6, 59.0, and 110.9-years frequency components in the Hongyuan δ¹⁸O_{tree ring}series, which may be the responses to solar activities, synchronize well with those recorded in other ISM indices. A notable feature of the reconstructed ISM intensity is the gradually decreasing trend from about 1860 to the present, which is inversely related to the increasing temperature trend contemporaneously. Such “decreasing ISM intensity–increasing temperature” tendency can also be supported by ice core records and meteorological records over a wide geographic extension. The decrease in sea surface temperature gradient between tropical and north Indian Ocean, and the decrease in land-sea thermal contrast between tropical Indian Ocean and “Indian sub-continent–western Himalaya” are possibly responsible for the observed decreasing ISM trend.