
September 09, 2010
From farmers to government officials in charge of efficiently managing
Earth's precious water and energy resources, people all over the world
rely on accurate short-term climate forecasts on timescales ranging
from a few weeks to a few years to make more informed decisions. But
today's climate forecast systems have limited ability to operate on
such timescales. That's because it's difficult to realistically
represent the complex interactions between Earth's ocean, atmosphere
and land surface in the climate models from which forecasts are
developed...
A new report by the National Academy of Sciences looks at the current
state of these climate predictions and recommends strategies and best
practices for improving them. Duane Waliser, chief Earth scientist at
NASA's Jet Propulsion Laboratory, Pasadena, Calif., was on the
12-member panel that conducted the NOAA-requested study.
Among the report's key recommendations:
- Continue research to better understand and use information from key
sources of climate predictability, and interactions between the ocean
and atmosphere, atmosphere and land, as well as volcanic eruptions,
greenhouse gases and land use changes.
- Improve the basic building blocks of climate forecasts through
better physical climate models, making more sustained physical
observations, better incorporating observations into forecast systems,
and increasing collaboration between forecast agencies and stakeholders
in developing and implementing forecast strategies.
- Adopt best practices such as working more closely with research
communities, particularly universities; making data that feed into and
come out of forecasts publicly available; minimizing subjective
forecast components; and using forecast metrics that better convey to
the public the probability aspects of forecasts.
Waliser contributed his expertise in a phenomenon called the
Madden-Julian Oscillation that exerts a powerful influence on
short-term climate predictions. During this type of climate pattern,
unusual variations of clouds, rainfall and large-scale atmospheric
circulation move slowly eastward from the tropical Indian Ocean into
the Pacific Ocean over the course of weeks, ebbing and flowing like
waves in cycles lasting about 40 to 50 days. This climate pattern
typically spans more than half the distance around Earth's equator. In
the disturbed portion of the "wave," air rises, triggering showers and
thunderstorms; in the sinking portion, air subsides, inhibiting clouds
and rainfall.
Madden-Julian Oscillation events can strongly influence long-term
weather patterns and have widespread impacts around the globe. They can
help trigger the beginning and end of the Asian and Indian monsoons and
influence the development and evolution of El Niño, hurricanes
and weather in Earth's mid-latitudes. Scientists want to incorporate
information about the oscillation more accurately into the climate
models that agencies around the world use to predict weather and
climate.
"Ten years ago, our ability to forecast Madden-Julian Oscillation
events was very limited," said Waliser. "Today, numerous operational
forecast centers around the world are recognizing the importance of
forecasting the MJO and are beginning to provide useful forecast
information about it. This information, in turn, can be used to make
better forecasts of other weather and climate phenomena.
"This new report highlights the key shortcomings and strategies needed
to make more accurate climate forecasts-- not just of the Madden-Julian
Oscillation, but of intraseasonal to interannual climate forecasts in
general," he added.
The full report, called "Assessment of Intraseasonal to Interannual
Climate Prediction and Predictability," can be read and downloaded at:
http://nationalacademies.org/morenews/20100908.html .