by Richard Anthes, UCAR president
There was no escaping climate change in 2007. The
topic took center stage throughout the year,
from record warmth in midwinter to the stunning loss
of Arctic sea ice last summer (see sidebar) to the
Nobel Peace Prize in the fall. The past year’s
reports from the Intergovernmental Panel on Climate
Change (IPCC) make it clear that our planet is warming
at an unprecedented rate and that human beings are
the major cause. We are heading into an unknown climate,
where weather patterns will change significantly over
those we have come to know, expect, and coexist with.
We
already know enough to begin taking action on
two important fronts: mitigation (reducing emissions
to reduce future climate change) and adaptation
(reacting to current changes and preparing society
for predictable and unforeseen changes that are sure
to occur no matter what we do). However, that knowledge
is no reason to reduce basic and applied research in
climate, weather, human interactions, and related areas.
In fact, just the opposite is true! The more we can
extend and deepen our knowledge about climate change,
the more efficient and effective our mitigation and
adaptation will be.
Understanding the complex,
changing planet on which
we live, how it supports life, and how
human activities affect its ability to
do so in the future is one of the greatest intellectual
challenges facing humanity. It
is also one of the most important challenges
for society as it seeks to achieve prosperity,
health, and sustainability.
Earth Science and Applications from Space: National
Imperatives for the Next Decade and Beyond (National
Research Council, 2007,
www.nap.edu/catalog.php?record_id=11820)
In spite of remarkable progress
over the past several decades, our understanding
of the complex physical, chemical, and biological
Earth system and its interactions with humans remains,
on many levels, rudimentary. We’ve
identified many research questions where there
is more that we don’t know than we do. And there
are certainly still more questions we don’t yet
even know we should be asking. Even the feedbacks
in the Earth system that we recognize as important
in a qualitative way are just beginning to be understood
in quantitative ways that can be included in
weather, climate, and Earth system models. As emphasized
in the recent National Research Council (NRC) survey
of space-based observations (see box above), understanding
of Earth and its inhabitants is indeed one of
humankind’s
greatest intellectual challenges, and this alone
makes additional research an imperative.
Those who doubt
the importance of climate change will cite the
gaps in our understanding as reasons to slow down or
hold off action. Yet stressing the need to learn more
is not the same as discounting what we already know
from decades of research on greenhouse gases and their
effects. For example, a National Academy of Sciences
report in 1979 (often called the Charney report after
its leader, Jule Charney) estimated that a 3°C (5.4°F)
warming could result from a doubling of carbon dioxide.
This is actually not far off the mark: Earth’s
surface atmosphere has warmed about 0.75°C (1.35°F)
in the last century as CO2 concentrations have risen
by about 30%.
The fundamentals: observing and computing

Rick Anthes.
(Photos by Carlye Calvin.)
We may know with near-certainty that the climate will
continue to warm over the next century, but the
odds on whether it might warm a more-or-less-manageable
1°C (1.8°F) or a potentially catastrophic 5°C
(9°F) or more are not known with confidence. As
for moisture, one of the important conclusions
of the 2007 IPCC report was that most subtropical land
areas are likely to receive less precipitation, while
high latitudes are very likely to receive more. The
signal is not so clear across some other regions, though,
including much of the United States.
In order
to monitor, understand, predict, and adapt to
climate change—including the all-important
changes in extreme and impactful weather on local
and regional scales, where it really counts—we
have a long way to go. Now more than ever, we
need better Earth observations, increased computer
power to process the observations and run the models,
improved weather and climate predictions, and enhanced
research on how weather and climate affect social order
and life on the planet.
Calls for more funding are
a familiar aspect of science. What many observers
may not realize is that, in recent years, the
nation’s
investments in the key areas listed above have
been decreasing in real dollars.
For example, observations
of the entire Earth—its
atmosphere, oceans, land, and ice surfaces—are
the foundation for improved understanding of
climate change and for computer models that accurately
predict weather and climate. Yet the number of
space-based sensors for monitoring Earth’s atmosphere
will drop by 50% by 2015, due to budget reductions
and shortfalls at NASA and NOAA. Imagine flying
an airplane into uncharted territory during a storm
with half of its instrument panel gone dark. To make
our way through a changing climate, we cannot afford
to fly half-blind.
There is also no substitute for computing
power to understand and predict weather and climate.
Larger and faster computers allow scientists
to effectively combine the suite of diverse global
observations into a meaningful whole and to make
predictions and warnings with increasing accuracy
and detail for local areas. Ever more powerful
computers will be needed to build and run Earth
system models that contain biological and chemical
processes and human interactions. These advanced models
will be essential tools in both understanding
and predicting climate change and in societal demands
for information. Yet computing power at major climate
modeling centers such as NCAR is increasing in a business-as-usual
way that does not reflect the importance of the
science and the need for vastly improved decision support
tools related to climate and weather.
The recent
downturn in support for basic observing and computing
systems puts us at increased risk as we move
forward into a very uncertain world, one in which the
timing, frequency, and intensity of a whole range of
phenomena—from
droughts and heat waves to forest fires and hurricanes—are
in question.
Seeking new types of answers to burning questions
Beyond the intellectual challenges they pose, climate
and weather changes stand to affect almost every part
of our society: public health and safety, economic
and social stability, agriculture, water supplies and
management, energy production and use, transportation,
and military readiness. In each of these areas, policy-
and decision makers are clamoring for concrete guidance
on what to expect as our climate and weather evolve
and how to adapt to changes. For example:
• What kinds of crops are best suited to hotter,
more drought-prone areas?
• How might rising sea level, intensified
rainfall, and changes in hurricanes affect cities along
the Gulf and Atlantic coasts?
• How long will it take for the Arctic Ocean
to experience ice-free conditions in summer?
• How will energy and water demands and
supplies change in my city, state, or region?
Surprises at both poles

As large parts of the Wilkins Ice Shelf
disintegrated, they broke into a sky-blue pattern of
exposed deep glacial ice. This true-color image of the
Wilkins Ice Shelf was taken by NASA’s MODIS (Moderate
Resolution Imaging Spectroradiometer) on 6 March. The
Wilkins shelf is located on the Antarctic Peninsula,
farther from the South Pole than most of Antarctica.
(Illustration courtesy National Snow and Ice Data Center.)
The northern and southern polar regions continue to serve
as bellwethers of climate change. As
reported last fall in the UCAR Quarterly (www.ucar.edu/communications/quarterly/fall07/arcticmelt.jsp),
sea-ice coverage in the Arctic Ocean
fell to dramatic new lows last summer. The graphic on page
5 illustrates how much this drop exceeded the range of
model projections for the past few years. Aside from the
obvious message that Arctic ice is melting rapidly, there
is another important lesson. Skeptics often discount climate
change projections that seem alarming, but we must remember
that these model projections, especially on regional scales,
also have the potential to be too conservative, as in this
prediction of Arctic sea ice.
In the Southern Ocean adjoining
Antarctica, the winter of 2007 saw the
greatest sea-ice extent on record, although
the 2007 IPCC report notes that no significant change has
been observed over the time scale of recent decades. A
little farther away from the
pole, along the Antarctic Peninsula—the fastest-warming
region on Earth—glaciers are showing increasing signs
of instability. In March 2008, scientists
from the U.S. National Snow and Ice Data Center, the British
Antarctic Survey, and Taiwan’s Earth Dynamic Research
Center announced the rapid deterioration of the Wilkins
Ice Shelf, which is roughly the size of Connecticut.
During
the month of March, a large iceberg fell
away from the seaward edge of the Wilkins shelf, which
led to disintegration of some 405 square kilometers (160
square miles) of ice (see image). In 1993, British Antarctic
Survey scientist David Vaughan had predicted such a collapse
but thought it could take up to 30 years to unfold. The
rest of the Wilkins Ice Shelf—the largest one
in West Antarctica threatened to date
by a warming climate—is
now protected from the sea by a strip of ice only
6 kilometers (3.7 miles) wide.
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In addressing these and other key questions, scientists
must provide quantitative as well as qualitative information
at increasingly regional and local scales. We
need to work with users to understand what might happen,
what will almost certainly happen, and where the science
has yet to support firm conclusions. With increased
computing and modeling power, we can expand the type
of ensemble climate modeling systems that are beginning
to tackle questions on the regional level, such as:
• What scenarios are possible? Most likely?
• What are the worst and best cases?
• What are the probabilities of the different
scenarios?
• How can we quantify the risks associated with
various contemplated courses of action?

In a set of model runs produced for the 2007 IPCC assessment, the NCAR-based Community Climate System Model projected that the Arctic Ocean’s summer sea ice would began a sharp decline in coverage during the 2010s. However, the decline from 2000 through 2007 in September ice extent (blue trace) exceeded the projections of any member of this ensemble (ensemble range in yellow, mean in red). (Illustration courtesy CCSM and Marika Holland.)
Meteorologists and social scientists are exploring
new types of probabilistic weather prediction
(see article, page 10). Society will need similar tools
on the much longer time frames of climate prediction.
As for mitigating climate change, there are many ways
for individuals and organizations to reduce emissions
now, as discussed in my fall 2007 column (www.ucar.edu/communications/quarterly/fall07/president.jsp).
There is also growing research and popular interest
in bio- and geoengineering techniques for reducing
or sequestering emissions on a regional or global
scale. These proposals include techniques as
varied as afforestation (creating new forests
in long-treeless areas), growing biofuels of many types,
placing mirrors into orbit, or injecting reflective
aerosols (particles) into the atmosphere. The lessons
learned from the checkered history of weather modification
should be heeded here; unintended consequences
may be much more severe when it’s the global
climate that is being intentionally modified.
As we
consider adaptation and mitigation, we need to
be fully aware of important assumptions that may go
unacknowledged yet can influence our views of the future
profoundly. For example, the IPCC climate scenarios
are powerful and sophisticated tools. They take into
account various potential changes in population, the
economy, technology, and fuel use in depicting how
the next century of emissions and associated climate
change could unfold. Yet, as pointed out by several
researchers in a recent Nature commentary (see article,
page 3), the IPCC scenarios implicitly assume that
the bulk of the challenge of reducing future emissions
will occur in the absence of climate policies, an assumption
that may be optimistic. If policymakers fail to take
these assumptions into account, they may underestimate
the challenges that lie ahead. It’s not enough
for Congress, state and local governments, and
corporations to be aware of climate change: they must
have as firm a grasp as possible on likelihoods, probabilities,
and possibilities.
Caution: science under construction
Our current ideas on how to deal with climate change
rest on a scientific foundation that remains
only partially built. Especially when it comes to large-scale
mitigation efforts, we may know just enough to be dangerous.
People will inevitably make choices based on today’s
far-from-complete scientific knowledge (society
cannot stand still while we do our work), but we must
learn more.
Enhanced observations of Earth are needed
to validate and improve climate models, support
more accurate and precise predictions, confirm or deny
these predictions, and detect surprises. Physical as
well as social scientists must listen to stakeholders,
map out our vulnerabilities to extreme weather, and
learn how to increase society’s
flexibility and resilience in the face of a climate
never before experienced by humans. And we must
develop the advanced models that can greatly improve
our forecasting and warning systems and sharpen our
look into the future.
Will we as a community be able to meet these
national needs? As a result of budget battles
between the White House and Congress, federal
funding for climate, weather, and other Earth science
research at NASA, NOAA, and NSF will drop in real terms
this year—for
the fourth year in a row—while our ability to
monitor Earth’s vital signs begins to decline.
Future leaders in the White House and Congress will
be forced to juggle many priorities. If climate
change ranks among the top threats facing our planet,
as I and many others believe, then it seems imperative
that we invest in observing, understanding, and predicting
our climate at a level commensurate with the
risk we face, while at the same time carrying out unprecedented
mitigation and adaptation efforts on a local,
national, and global basis. ♦
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