Category Archives: Daily Measurements

Note on Pause in Daily Readings

Readings of CO2 from Mauna Loa have been unavailable for two weeks.

According to technicians with the Scripps CO2 Group, the problem is a disk failure that handles the data buffering, which has broken the data stream and valve switching that impacts daily calibration.  The air data are recoverable, because the computer onboard the actual instrument is still working and taking air data, but we will need to assess the stability of calibration once the instrument is working completely again.  A replacement was shipped last week, so it should be up again shortly.

– Robert Monroe

 

Why Don’t Global Surface Temperature Trends Match Atmospheric CO2 Increases?

LARGE_KC400_YassirQuestion submitted to Scripps Oceanography science magazine explorations now by Ruben M., Watsonville, Calif.

Great question Ruben! The surface temperature we experience every day is not expected to perfectly track CO2 because CO2 isn’t the only factor driving climate change. Still, it is quite an important factor, and the overall rise in temperature does roughly follow the overall rise in CO2.

The temperatures we experience every day reflect only a portion of the solar energy absorbed by the earth. For instance, the long-term warming effects of CO2 and other greenhouse gases are largely buffered by the ocean, which absorbs more than 90 percent of the excess heat caused by human emissions of CO2 and other greenhouse gases.

Furthermore, human-caused warming is superimposed on a naturally variable climate system, driven by various dynamic processes and events that influence the temperatures we experience.

Because CO2 can remain in the atmosphere for a century or longer, its increasing concentration due to human activities warms our climate over long periods of time. Through its absorption and emission of energy back onto Earth’s surface, increased atmospheric CO2 traps more heat in the climate system. Its warming effect, however, is simultaneously amplified and dampened by positive and negative feedbacks such as increased water vapor (the most powerful greenhouse gas), reduced albedo, which is a measure of Earth’s reflectivity, changes in cloud characteristics, and CO2 exchanges with the ocean and terrestrial ecosystems.

Shorter-lived greenhouse gases and particles such as methane and black carbon emitted by human activities also contribute to observed trends in global mean temperatures. Some air pollution particles, such as sulfates, can have cooling effects through their reflection of incoming solar radiation. 

The gradual warming of the climate system caused by human activities is superimposed on natural phenomena such as El Niño Southern Oscillation, a climate cycle driven by changes in atmospheric and ocean circulation and sea surface temperatures in the equatorial Pacific. Similar but longer-term natural variability can also influence global mean surface temperature trends over several decades, as Scripps researchers have recently reported.

Also, volcanic eruptions such as that of the Philippines’ Mt. Pinatubo in 1991 can cool the planet for a few years by adding sulfate particles into the stratosphere, reflecting solar radiation back to space.

Finally, the 11-year solar sunspot cycle can cause fluctuations in the global temperature record that may not be as visible amid the numerous human and natural factors regulating our complex climate system. Global mean surface temperatures are only one way to assess the full impact of fossil fuel emissions and they do not reflect the regional aspects and ever-growing complexity of our changing climate.

– Yassir Eddebbar is a third year doctoral student in the Scripps CO2 Laboratory, Climate-Ocean-Atmosphere Program

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