A New Kind of Climate Model Project

Many scientists these days are asking how they can better communicate their research to the public. One group of climate researchers has found a solution–by putting themselves into the spotlight (literally) in the 2014 Climate Models wall calendar.
Scheduled for release this December, the calendar will include pictures of 13 climate scientists as well as information about them, such as their favorite dataset or climate phenomenon. Their ultimate goal, according to their website, is to “increase awareness of climate change and its impacts by engaging the public with scientists and what they’re learning about Earth’s climate.” In the process, the scientists reveal a side of themselves that most of the public doesn’t regularly get to see, and they hope to inspire colleagues to be equally creative in sharing their research with the public. You can get a sneak preview of a few of the models in the video below.
In addition to their work in front of the cameras, the scientists, who represent Columbia University’s International Research Institute for Climate and Society and Lamont-Doherty Earth Observatory, and the NASA Goddard Institute for Space Studies, will also be presenting a poster about their novel communication efforts at December’s AGU Fall Meeting in San Francisco.
You can help support the calendar by donating to its Kickstarter campaign.

Share Ideas on Climate, Influence Policy Options

The Front Page received the following note from John Nielsen-Gammon, Regents Professor of Atmospheric Sciences, Texas A&M University; Texas State Climatologist; and a Fellow of AMS:

A Message To Fellow Physical Scientists
I’m part of a new journalistic endeavor called the Climate Change National Forum and Review.  The purpose of this web site will be to provide a public forum wherein scientists can discuss the latest research on climate change and share and debate ideas on aspects of climate change especially relevant to policymaking.  When the second phase kicks in, policy experts will join the discussion and compare the benefits and costs of possible responses.
I know what you’re thinking: “This sounds an awful lot like the IPCC.”  Well, it’s not.  Nor is it intended to replace the IPCC in any way.  It has a different purview and a different set of goals.

  • The IPCC is an international body. The CCNFR is focused on issues facing the United States.
  • The IPCC scientists are selected from nominees from various countries. The CCNFR scientists consist of anyone who contributes regularly and constructively to the discussion.
  • The IPCC produces reports every few years, whose summaries are edited and ratified by political representatives. The CCNFR web site is a living document, continuously updated to account for the latest science, and not subject to political interference.
  • The IPCC’s purview is anthropogenic climate change. The CCNFR’s purview is climate change in all its causes and manifestations.  Would it make sense to only adapt to anthropogenic climate change?
  • The IPCC reports are written by experts within their subject fields. The CCNFR will draw upon the expertise and experience of scientists from a wide range of fields, not just insiders.
  • The public gets to see the IPCC final report. The public gets to see scientists grappling with, understanding, and debating the issues.

For me, this last point is an important one.  The public can benefit tremendously from being able to see how scientists think and reason scientifically.  We ask them to trust our collective scientific wisdom without allowing them to see how we evaluate conflicting or flawed evidence and develop judgments.  Presently, the only extensive example of this available to the public is the set of emails from Climategate.
Why should you participate?  First, you’ll gain a deeper understanding of climate science.  Perhaps you’ve just taken the IPCC reports on faith, trusting the experts to do a good job.  Whether they did or not, you will be better able to articulate the issues and explain them to others after exchanging ideas, digging into some of the primary literature, and fleshing out any questions that might be nagging you in the back of your mind.
It should be obvious by now that you don’t need to be a climate scientist to participate, as long as you have a suitable technical background.  Indeed, we need at least some people who know relatively little about the state of the art of climate science, for their intellectual journey while participating in the CCNFR is similar to the journeys we hope dedicated lay readers will take.  Outsiders to climate science can better spot the unspoken assumptions and unjustified conventions.
Your learning will come through the course of online debate and discussion with other scientists.  As you probably know from personal experience, discussion with other scientists is often the absolute best way to come to grips with a contentious or controversial scientific issue.  Along the way, you will develop skills as a writer for an outside audience.
Finally, you will be doing a public service, simultaneously helping to educate the public about climate change and about science in general.
On the negative side, it requires time, though not a whole lot.  We’re only asking for participants to contribute new essays once a month, plus participate in some of the online discussions with other scientists.  Compared to starting your own blog, this is a relatively easy way to bring your ideas and judgment into public view.
Scientists who think they know everything about climate change are not welcome to participate.  If you’re an expert in a particular branch and want to broaden your knowledge, or even if this is something outside your expertise entirely so that you have a lot you want to learn, then come join us.

The link above that John provides is a beta form of the CCNFR web site. To facilitate your postings explaining, debating, and discussing climate science–and to keep the site tied to issues in the news and policymaking–the CCNFR hopes to provide a steady stream of news and statements culled even-handedly  from the media by a professional journalist.
As such, this is not only a time to consider getting in on the ground floor of a new public outreach project but also a time to consider making a donation. The CCNFR hopes to raise more than $60,000 to get a journalist on board soon.

The President's Climate Speech

by Paul Higgins, AMS Policy Program Director
In June, President Obama gave a long-anticipated speech laying out his vision for climate change risk management. The centerpiece of the approach is to use the EPA to regulate greenhouse gas emissions from power plants. What those regulations will look like remains unclear, but the President’s intent to reduce emissions significantly, particularly from coal-fired power plants, is clear.
By all accounts, this wasn’t the approach the president wanted to take for climate change. He has said repeatedly and throughout his presidency that he favors a bipartisan solution that comes from Congress. After nearly five years and with the end of his second term approaching, the president appears to have concluded that the political divisiveness surrounding climate change makes congressional action unlikely.
How well the president’s approach will work is hard to know, of course, but it will be particularly interesting to see how this unilateral effort affects the politics of climate change risk management. There is a chance that the president’s plan will ultimately reduce the political divisiveness surrounding climate change, in part, because the approach itself is politically divisive.
Using the EPA to regulate emissions will not go over well with many in Congress. His opponents will likely find it easy to criticize, and score political points in so doing, on both philosophical grounds (i.e., based on a preference for less intrusive federal intervention) and because unilateral executive action is less democratic than including Congress in the creation of a new law. But the very fact that substantive arguments can be made for different approaches may provide an incentive for his opponents to develop and offer those alternatives. That could create an important opening that’s been largely missing for climate change over the last few decades.
Prior to the 1990, Clean Air Act Republicans and Democrats could more easily agree on an environmental problem yet disagree on the solution. Republicans tended to prefer market-based solutions while Democrats tended to prefer command-and-control regulation. Conservative philosophy convincingly won that debate because the market-based approach used in the 1990 Clean Air Act proved far superior as a tool for protecting the environment and maximizing the economic benefits of doing so.
Perversely, that philosophical victory for conservatives has made it harder for the two parties to agree on climate change risk management. There isn’t an easy way for the parties to distinguish themselves if they agree on the basics of the solution. Instead, the political incentive has been to disagree about whether there is a problem in need of a solution in the first place. Once the champions of climate policy coalesced on a conservative approach for addressing climate change, the choice for everyone else became too stark: go along with that approach or oppose climate policies altogether. If there isn’t middle ground and your opponent is for it, then few options are more politically effective than being against it.
Of course, the politics of climate change are, and will likely continue to be, challenging for other reasons, most notably because of the competing and incompletely reconcilable interests of those affected by policy options. But there is a wide range of potential solutions for helping to manage climate change risks. Critically, there is a policy option for virtually any political philosophy out there. For example, Congress could use a market-based approach to reduce greenhouse gas emissions while simultaneously using every penny that the government raises through such an approach to reduce existing taxes on wages, corporate income, or capital gains. The reduction in taxes that would result would be a major victory for conservatives that many Democrats could plausibly go along with. Yet such options haven’t been developed or seriously considered.
That a broad range of potential risk management strategies hasn’t been developed and explored by policy makers is a major breakdown in our policy process. That policy deliberations (and public debates) about climate science are routinely at odds with the assessments of the relevant subject matter experts is a major failure of our national dialogue on the topic.
These failures have resulted, in part, because the political incentives for developing and exploring policy options have been too weak. By moving to circumvent the current political impasse to climate policy through a unilateral approach (particularly one likely to face sharp political opposition), the president may create a new opportunity for a broader consideration of options. If that happens, whether or not the president’s proposed solution is sufficient, he may help to depolarize the politics of climate change and spur the consideration of new and meaningful approaches to climate change risk management.
AMS Policy Program Director Paul Higgins’s perspectives, including this column, will be appearing regularly in the Bulletin of the American Meteorological Society.

Crowdsourcing the Search for Carbon Dioxide Emissions



According to Arizona State University (ASU) Professor Kevin Gurney, there are approximately 30,000 power plants throughout the world, and collectively they account for close to half of all fossil-fuel CO2 emissions. As a modeler of these emissions, Gurney is trying to learn as much as possible about every one of the plants. Where are they? What kind of fuel does each plant use? How much CO2 does each one release into the atmosphere?
Obtaining this kind of data, however, is a monumental task. There is no worldwide database with all of the power plant information Gurney is looking for, and even after enlisting a number of undergraduate students in his lab to scour Google Earth for the locations of the largest plants, in six months they were able to identify the locations of only 500 across the globe. Realizing that the effort was “like looking for 25,000 needles in a giant haystack,” as Gurney described it, he has now taken another approach by creating an online game that utilizes contributions from the general public to pinpoint the locations of power plants and hopefully quantify the amount of CO2 each releases into the atmosphere.
The project is called Ventus, which is Latin for “wind.” In the game, players are asked for four pieces of information: the location of the power plant (within a few hundred meters), the type of fuel used at the plant, the amount of electricity the plant generates, and the amount of CO2 that is emitted from the plant. Participants in the game can contribute as much information as they have by placing pins on a Google map at the location(s) of the plants. When the game is completed in 2014, the person who contributed the largest amount of useable information will be declared “Supreme Power Plant Emissions GURU!” and will receive a trophy, as well as be a coauthor on a scientific paper about crowd-sourcing in scientific research.
“Our logic is that for every power plant in the world, there are probably at least a dozen people who live near it, work at it, or know someone who works at it” explained ASU’s Darragh O’Keefe, who built the website. “With the proliferation of phones and GPS, it makes it pretty easy to locate things.”
Early response to the game was enthusiastic, with Gurney reporting that people had logged on from almost every country in the world within a day of its mid-May launch.
“I’m always surprised by how fast this type of thing moves around the planet,” he told the Los Angeles Times.

Avoiding Toaster Strudel Exchanges

by Keith L. Seitter, CCM, AMS Executive Director
Those of us who have siblings know that the relationship is built, in part, on needling.
When my two sons, Kevin and Matt, were eight and three years old, respectively, Kevin enjoyed Toaster Strudel® as an occasional breakfast treat. Matt, meanwhile, was just beginning to learn the joys of thoroughly annoying a sibling and was quickly becoming quite good at it.  One weekend morning, the following exchange took place:

Matt (to Kevin): We don’t have any Toaster Strudel.
Kevin:  Yes we do.
Matt:  No we don’t.
Kevin:  We do.  Mom picked some up at the store.
Matt:  No we don’t.
Kevin (becoming annoyed):  Matt, we do have some, I saw mom put it in the freezer!
Matt (remaining completely calm and collected):  No we don’t.
Kevin (stomping to the freezer and pulling the box out):  See!  We do have it!
Matt (still calm and collected):  No we don’t.

At about this point, when Kevin was clearly exasperated, I think I did the parental thing and intervened to calm things down.
I relay this little story because some of the “debate” on climate change seems to be taking on the character of this Toaster Strudel exchange.  And it is far less amusing when it is happening among adults in the media and in the blogosphere.
Frequent readers of my monthly column in BAMS will know that I have long been advocating for open and respectful dialogue on the science of climate change, with all parties recognizing that as scientists it is our job to be skeptical and require solid theory and evidence to back up claims.  We must always be cognizant of how hard it is to keep our intrinsic values from triggering confirmation bias as we review research results or listen to alternative explanations for observational evidence.  Our training as scientists, however, makes it clear that our goal must always be the objective truth — whether it supports our belief system or not.  We must all strive for that level of integrity.
I continue to feel that with open and respectful dialogue on the various complex issues involved in climate change we can achieve greater understanding within our community and less divisiveness.  We have to recognize, however, that “Toaster Strudel exchanges” are not about the evidence.  They have an entirely different goal from finding the objective truth, and failing to recognize that will only lead to frustration.
 

State of the Union Address Sets Stage for Senate Climate Hearing Today

If, last night, you made it through the usual State of the Union appeals to bipartisanship, tax reform, health care, job creation, deficit control, and industrial revitalization–then you heard President Obama’s unusually blunt promise to take action on climate change.
And all you had to do was wait through the rest of the night before Congress started working on its response. The Senate Committee on Environment and Infrastructure, chaired by Senator Barbara Boxer, has already lined up a session on the “Latest Climate Science” for this morning, at 10 a.m. EST. The blue-ribbon panel of invited experts providing testimony includes AMS President J. Marshall Shepherd and you can follow the live webcast of the hearing at the committee’s website.
The hearing originally looked like a relatively routine overview of science following the release of the newly drafted National Climate Assessment, but now it is charged by the President’s new resolve to begin dealing with climate change, with or without Congressional input. His position was staked out in a few sentences hunkered down amidst a flurry of points about energy efficiency and independence:

[O]ver the last four years, our emissions of the dangerous carbon pollution that threatens our planet have actually fallen.
But for the sake of our children and our future, we must do more to combat climate change.
Now, it’s true that no single event makes a trend. But the fact is, the 12 hottest years on record have all come in the last 15. Heat waves, droughts, wildfires, floods, all are now more frequent and more intense. We can choose to believe that Superstorm Sandy, and the most severe drought in decades, and the worst wildfires some states have ever seen were all just a freak coincidence. Or we can choose to believe in the overwhelming judgment of science and act before it’s too late.
Now, the good news is, we can make meaningful progress on this issue while driving strong economic growth. I urge this Congress to get together, pursue a bipartisan, market-based solution to climate change, like the one John McCain and Joe Lieberman worked on together a few years ago.
If Congress won’t act soon to protect future generations, I will. I will direct..I will direct my cabinet to come up with executive actions we can take, now and in the future, to reduce pollution, prepare our communities for the consequences of climate change, and speed the transition to more sustainable sources of energy.

The threat of unilateral Executive action set off a storm of commentary (e.g., Exhibit 1, Exhibit 2) and is sure to put the Senate in a very different frame of mind for today’s hearing. As for the science of climate change and its impacts–the focus of the hearing–this morning’s line-up of guests undoubtedly will have plenty to say about the latest findings. For example, Prof. Donald Wuebbles of the University of Illinois, and Dr. John Balbus, of the National Institutes of Health, are among the lead authors of the 2013 National Climate Assessment (available for comment). Meanwhile, Dr. Shepherd has been speaking out frequently on both the impacts of climate change on society and on the scientific approach to evaluating the effects of climate change on extreme events, and of course he is part of the AMS Executive Council that updated the Society’s information statement on climate change in 2012.

A Chat with the Iceman

Thorsten Markus, on sea ice in Antarctica.

By Maureen Moses, AMS Education Program
I hope you all had a good Earth Science Week last week! The theme was “Careers in the Earth Sciences,” and the AMS Education Program participated in a twitter chat with NASA Polar Scientist Thorsten Markus, who admits that as a high schooler in Germany science wasn’t his passion, but becoming a musician was. Now head of NASA Goddard’s Cryospheric Science Lab, Dr. Markus makes measurements of ice thickness in Antarctica.
Chat participants included a whole classroom full of eighth graders. Dr. Markus had plenty of advice on how a future polar scientist with an adventuresome streak can make a splash in a cool field! Here are some of the questions he fielded–edited and excerpted from the full chat archived on Twitter:

I’m here with 25 8th grade Earth Science students and one student would like to know what the day to day duties are as a polar scientist.
It’s extremely playful — playing with lots and lots of satellite data and learning something new every day.
Do you get to travel to cool places or are you processing data in an office?
Oh man, yes. I used to go to the Arctic and Antarctic and also flew over them in helicopters and planes.
What was your favorite experience in the field as a scientist?
Seeing the penguins coming out of the water and then standing right next to us. Fantastic!
When you decided becoming a rock star might not happen, why did you choose physics over math for a major?
Physics is pretty much applied Math — you deal with everyday problems… and actually learn how to solve some.
Which class helped you the most to get where you are today?
Maybe Math, but the arts fostered my creativity, for thinking outside the box
What level math did you have to go to? (for the future polar scientists out there). THX for the response!
I have a Ph.D. in physics, which involves a lot of math — but there’s also chemistry, biology and geography.
What is the difference between glacier ice data and sea ice data… Do they tell different stories?
Very different. Glacier ice is fresh water from mountains or ice sheets whereas sea ice is frozen ocean.
Are they affected differently by climate change?
Glaciers are balanced by snowfall and temperature, while with sea ice, also ocean properties play a big role.
So sea ice is inherently more volatile/variable?
I’d like to say sea ice is more complex, but then the ice sheet people might get angry 😉
What is/will be the impact of disappearing ice sheet on the global climate?
Melting of the ice sheets will increase sea level and affect ocean circulation because of the fresh water influx.
When can we expect to see Antartica’s ice retreating because of climate change. If it keeps stable or increasing, what can be made of that?
The Arctic and Antarctica are two different systems and global warming does not mean it warms uniformly everywhere.
What do you say to people who claim there’s a “debate” about climate change?
I don’t think there’s a “debate” about whether there’s climate change. The debate is by how much we’re responsible for it.
How good are the current models in predicting Arctic and Antarctic ice response to the climate warming?
I think the models are remarkable — certainly not perfect, but what prediction is perfect?
What climate data scares you the most (has the greatest implication for scary future events)?
The global ocean circulation, because it shows that things we do to the Chesapeake Bay may affect far away places.
Does any of the research you do tell us anything about other sheets of ice in cosmos?
As a matter of fact, I was involved in research about the Jupiter icy moons. So yes, there are analogies.
Who do you regard as your inspiration?
It was Keith Richards, now it’s the balance of the earth system… isn’t it remarkable how it all works together?
 

AMS Releases Revised Climate Change Statement

The American Meteorological Society today released an updated Statement on Climate Change (also available here in pdf form), replacing the 2007 version that was in effect. The informational statement is intended to provide a trustworthy, objective, and scientifically up-to-date explanation of scientific issues of concern to the public. The statement provides a brief overview of how and why global climate has changed in recent decades and will continue to change in the future. It is based on the peer-reviewed scientific literature and is consistent with the majority of current scientific understanding as expressed in assessments and reports from the Intergovernmental Panel on Climate Change, the U.S. National Academy of Sciences, and the U.S. Global Change Research Program.
“This statement is the result of hundreds of hours of work by many AMS members over the past year,” comments AMS Executive Director Keith Seitter. “It was a careful and thorough process with many stages of review, and one that included the opportunity for input from any AMS member before the draft was finalized.”
The AMS releases statements on a variety of scientific issues in the atmospheric and related sciences as a service to the public, policy makers, and the scientific community.

Climate and Weather Extremes: Asking the Right Questions

The still-developing field of attribution science examines specific weather events and short-term atmospheric patterns in a broader, longer-term climate context. In such research, communication is key; it’s vital to understand exactly what questions are being asked. A case in point is an article in the July issue of BAMS. “Explaining Extreme Events of 2011 from a Climate Perspective” gives long-term context to some of the significant weather events of 2011 featured in the new State of the Climate, which is also part of the July BAMS.
The authors write:

One important aspect we hope to help promote …is a focus on the questions being asked in attribution studies. Often there is a perception that some scientists have concluded that a particular weather or climate event was due to climate change whereas other scientists disagree. This can, at times, be due to confusion over exactly what is being attributed. For example, whereas Dole et al. (2011) reported that the 2010 Russian heatwave was largely natural in origin, Rahmstorf and Coumou (2011) concluded it was largely anthropogenic. In fact, the different conclusions largely reflect the different questions being asked, the focus on the magnitude of the heatwave by Dole et al. (2011) and on its probability by Rahmstorf and Coumou (2011), as has been demonstrated by Otto et al. (2012). This can be particularly confusing when communicated to the public.

So the new attribution paper in BAMS strives to answer a very specific questions–a series of them, as it turns out, since the paper is actually a collection of a number of studies by different teams, representing several of the cutting-edge approaches to researching attribution in rapid response to the extreme weather. Most of the authors, but not all, seek to answer questions about how global climate change changes odds that extreme events might occur.
Last week, NOAA held a briefing to discuss both the State of the Climate and the new BAMS article. Two coauthors of the article, Tom Peterson of NOAA’s National Climatic Data Center and Peter Stott of the Met Office Hadley Centre, discussed the answers they found. They noted that in some cases, such as the rainfall that caused flooding in Thailand, there was no connection between human activities and the extreme weather. But other events exhibited a clear human influence that increased the possibility of that event occurring. One example is the prolonged heat wave in Mexico and the southwestern United States, which was the region’s hottest and driest growing season on record by a significant margin. The steamy temperatures were connected to the La Niña that was prominent last year, and the study found that such a heat wave is 20 times more likely in La Niña years today than it was in 1960. As the coauthors noted in the briefing, the answer might be completely different in years without a La Niña , pointing out the importance of context–and understanding the questions being asked–in this study.
The State of the Climate itself documents the weather extremes of the recent past and give them context in the historical record. The 282-page peer-reviewed report, compiled by 378 scientists from 48 countries around the world, also provides a detailed update on global climate indicators and other data collected by environmental monitoring stations and instruments on land and ice, at sea, and in the sky. It used 43 climate indicators to track and identify changes and overall trends to the global climate system. These indicators include greenhouse gas concentrations, temperature of the lower and upper atmosphere, cloud cover, sea surface temperature, sea level rise, ocean salinity, sea ice extent, and snow cover. Each indicator includes thousands of measurements from multiple independent datasets.
Among the highlights of this year’s SOC:

  • Warm temperature trends continue: Four independent datasets show 2011 among the 15 warmest since records began in the late nineteenth century, with annually-averaged temperatures above the 1981–2010 average, but coolest on record since 2008. The Arctic continued to warm at about twice the rate compared with lower latitudes. On the opposite end of the planet, the South Pole recorded its all-time highest temperature of 9.9°F on December 25, breaking the previous record by more than 2 degrees.
  • Greenhouse gases climb: Major greenhouse gas concentrations, including carbon dioxide, methane, and nitrous oxide, continued to rise. Carbon dioxide steadily increased in 2011 and the yearly global average exceeded 390 parts per million (ppm) for the first time since instrumental records began. This represents an increase of 2.10 ppm compared with the previous year. There is no evidence that natural emissions of methane in the Arctic have increased significantly during the last decade.
  • Arctic sea ice extent decreases: Arctic sea ice extent was below average for all of 2011 and has been since June 2001, a span of 127 consecutive months through December 2011. Both the maximum ice extent (5.65 million square miles on March 7, 2011) and minimum extent (1.67 million square miles, September 9, 2011) were the second smallest of the satellite era.
  • Ozone levels in Arctic drop: In the upper atmosphere, temperatures in the tropical stratosphere were higher than average while temperatures in the polar stratosphere were lower than average during the early 2011 winter months. This led to the lowest ozone concentrations in the lower Arctic stratosphere since records began in 1979 with more than 80 percent of the ozone between 11 and 12 miles altitude destroyed by late March, increasing UV radiation levels at the surface.
  • Sea surface temperature and ocean heat content rise: Even with La Niña conditions occurring during most of the year, the 2011 global sea surface temperature was among the 12 highest years on record. Ocean heat content, measured from the surface to 2,300 feet deep, continued to rise since records began in 1993 and was record high.
  • Ocean salinity trends continue: Continuing a trend that began in 2004, and similar to 2010, oceans were saltier than average in areas of high evaporation, including the western and central tropical Pacific, and fresher than average in areas of high precipitation, including the eastern tropical South Pacific, suggesting that precipitation is increasing in already rainy areas and evaporation is intensifying in drier locations.

The report also provides details on a number of extreme events experienced all over the globe, including the worst flooding in Thailand in almost 70 years, drought and deadly tornado outbreaks in the United States, devastating flooding in Brazil and the worst summer heat wave in central and southern Europe since 2003.
 

Small Microbes Play Big in Climate Arena

Microbes may be small, but they shouldn’t be ignored when considering global climate.  According to a new colloquium report from The American Academy of Microbiology, microbes such as bacteria, algae, and fungi play a powerful role in the Earth’s climate.  “Incorporating Microbial Processes into Climate Models” notes how the impact of microbes on the atmosphere goes way back in time. The critical mix of carbon dioxide and oxygen we take for granted as sustaining life on the planet is due to the rise of these tiny creatures eons ago.
So what specifically do these minute forms of life have to do with climate today? According to the report, the answer is plenty.  “The sum total of their activity is enormous. But of course not all microbes are the same—some of them are producing oxygen, others are consuming it. Some are taking carbon dioxide out of the air, others are adding it.”
The big questions that the report asks and plans to address by incorporating microbial processes into climate change models: what’s the overall effect of microbial activities on the concentration of carbon dioxide in the atmosphere? Is it possible this activity will absorb the carbon dioxide being added to the atmosphere? Or will the rising global temperature might spur microbes to produce even more carbon dioxide?
The authors recognize that the gap between the climatology and microbiology is large, but they say it is not insurmountable. Some of the same technologies used to collect data for climate models—satellite imaging of cloud cover and precipitation, submarine cables that monitor changes in temperature and salinity, sensors to retrieve real-time data from remote locations—can also be applied to measuring biological phenomena. Collaboration between the sciences, they believe, will benefit both fields.
A more detailed look at the report is available here.