Showing posts with label El Nino. Show all posts
Showing posts with label El Nino. Show all posts

Wednesday, April 06, 2011

Faster sailing across the Central Pacific: Wind speeds and El Nino

The new paper by Young et al. about increasing wind speeds and wave heights over the past twenty years created a bit of a buzz in the climate science world, not to mention the sailing world. Finally some good news, the windsurfer in me first upon seeing the paper.

The paper itself does not speculate about whether human-caused climate change is the driver of the global trend in wind speeds. That may have been a wise choise, as it would be difficult, statistically or dynamically, to attribute the rend in the reasonably short time series (~23 years) to any single forcing factor.

The spatial pattern, however, is quite striking:














If there were no labels on this figure, I'd have guessed it was the trend in sea surface temperatures over the same time period. The steepest trend is in the Central Pacific, including the waters around the Gilbert and Phoenix Islands of Kiribati.

In a map of temperature trends over the past two to three decades, the Central Pacific should jump out because of the increasing frequency of "Central Pacific" El Nino events, also known as El Nino Modoki. The more freuqent occurences of the "CP" El Nino is a subject of much research, and has been attributed by some authors to climate warming. The CP El Nino is responsible for a number of mass coral bleaching events, including 2002-3 in the Phoenix Islands, 2004-5 in the Gilbert Islands, and 2009-10 across the whole region.

It is not surprising to find a similar -- at least visually, take this with a grain of salt, I've not done the statistics -- spatial pattern in the surface wind speeds across the Pacific. More frequent Central Pacific warm events likely means larger pressure gradients, more convergence, and higher winds across the region (my paper in  the Atoll Research Bulletin describesa CP El Nino event in relatively lay terms). More analysis will need to be done, but at first glance, the wind speed trends over the Pacific appear to be driven by temperature trends and the status of climate oscillations, which themselves may be driven in part by climate change.

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Monday, November 22, 2010

If a hurricane dies at sea, does anybody count it?

This post from the Capital Weather Gang is a reminder that the lack of Atlantic hurricanes which made landfall this year does not mean it was a tepid hurricane season. The year's tracks are shown at right.

The number of named Atlantic storms (19) and number of hurricanes (12) was twice the long-term average and higher than almost all of the predictions. The difference this year is that no powerful storms struck the U.S. thanks to the response of the upper-level air flow to the El Nino / La Nina oscillation in the Pacific, a subject discussed here before.

The Atlantic hurricane discussion tends to focus almost entirely on the U.S. It is important to remember that not every country was spared. Haiti (above) is still recovering from Hurricane Tomas, in particular the outbreak of cholera caused or exacerbated by the heavy rainfall and flooding just a few weeks ago.

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