Stronger Pacific winds explain global warming hiatus-study

LONDON, (Reuters) – Stronger winds which have cooled the surface of the Pacific Ocean could explain what is likely to be a temporary slowdown in the pace of global warming this century, researchers said.

Last year, scientists on the Intergovern-mental Panel on Climate Change (IPCC) said the pace of temperature rise at the Earth’s surface had slowed over the past 15 years, even though greenhouse gas emissions, widely blamed for causing climate change, have risen steadily.

Past research has linked the slowdown in the pace of warming to factors such as a build-up of sun-dimming air pollution in the atmosphere or a decline in the sun’s output. Others suggest the deep oceans may be absorbing more heat.

A study published in the journal Nature Climate Change on Sunday said stronger Pacific trade winds – a pattern of easterly winds spanning the tropics – over the past two decades had made ocean circulation at the Equator speed up, moving heat deeper into the ocean and bringing cooler water to the surface. The winds have also helped drive cooling in other ocean regions.

“We show that a pronounced strengthening in Pacific trade winds over the past two decades is sufficient to account for the cooling of the tropical Pacific and a substantial slowdown in surface warming,” said the study, led by scientists from the University of New South Wales in Australia.

“The net effect of these anomalous winds is a cooling in the 2012 global average surface air temperature of 0.1-0.2 degrees Celsius, which can account for much of the hiatus in surface warming since 2001.”