Revelle factor

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The Revelle factor (buffer factor) is the ratio of instantaneous change in carbon dioxide (CO2) to the change in total dissolved inorganic carbon (DIC), and is a measure of the resistance to atmospheric CO2 being absorbed by the ocean surface layer.[1] The buffer factor is used to examine the distribution of CO2 between the atmosphere and the ocean, and measures the amount of CO2 that can be dissolved in the mixed surface layer. It is named after the oceanographer Roger Revelle, who was one of the first scientists to study global warming.

Revelle factor = (Δ[CO2] / [CO2]) / (Δ[DIC] / [DIC]) where DIC is dissolved inorganic carbon. Δ[CO2] / [CO2] is the instantaneous change in pCO2 and Δ[DIC] / [DIC] is the instantaneous change in DIC.

Thermodynamics[edit]

In order to enter the ocean, carbon dioxide gas has to partition into one of the components of carbonic acid: carbonate ion, bicarbonate ion, or protonated carbonic acid, and the product of these many chemical dissociation constants factors into a "back-pressure" that limits how fast the carbon dioxide can enter the surface ocean.

DIC[edit]

The species of DIC present in ocean waters is dependent on the systems alkalinity, and is illustrated by the Bjerrum plot below (Figure 1). Carbonate is dominant in higher pH environments (basic), whereas carbon dioxide is dominant in lower pH environments (acidic). Bicarbinate ions are abundant in relatively mid-pH waters, with a range from four to ten. As the pH decreases, most of the DIC will be pCO2, and the buffer factor will increase.[2] An increased buffer factor results in a decreased buffering effect, which could lead to the uptake of more pCO2 from the atmosphere, and decreasing the pH even more.[2]

Figure 1: Figure 1 illustrates the molar fraction of carbonate species present in seawater across pH, with salinity set at 5,000ppm, and temperature set to 25 degrees Celsius. Note temperature and salinity effect carbonate species present, and vary with location and season.

Carbonate Bjerrum.gif

DIC and alkalinity govern carbonate and acid-base chemistry in the world’s oceans, and their effects on the Revelle factor is no exception. The ratio of DIC to total alkalinity, and the changes in pCO2 are the main cause of Revelle Factor variability. Higher levels of DIC result in a lower Revelle factor, and consequently a larger buffering effect.[3] Higher levels of pCO2 results in a higher Revelle factor, a positive feedback loop, and consequently a smaller buffering effect. Typically, the buffer factor ranges between 8 and 13.

Anthropogenic CO2[edit]

The capacity of the ocean waters to take up surplus (anthropogenic) CO2 is inversely proportional to the value of the Revelle factor. Hence, in modern-day oceans, it is possible to see the concentrations of anthropogenic CO2 by measuring the Revelle factor; the lower the Revelle factor, the greater the amount of anthropogenic CO2.[4] Low Revelle factors are typically found in the warmer tropical to subtropical waters, whereas higher Revelle factors are found in the colder high latitude waters of the North Atlantic. The North Pacific has higher Revelle factors, and has lower anthropogenic CO2. This is due to the fact that the alkalinity values in the North Pacific are as much as 100µmol kg⁻¹ lower than those in the North Atlantic.

The Revelle effect[edit]

The Revelle effect describes how only a small fraction of pCO2 is present in ocean water when much larger amounts are added to the atmosphere. Depending on the alkalinity of the water, DIC is either present as CO3, HCO3, or CO2. When the pH is high (basic) the Revelle factor is greatest, causing much of the DIC to exist as HCO3 or CO3, and not CO2. So, the greater the buffering effect (low Revelle Factor) the more DIC occurs as CO2 or HCO3, effectively lowering the pCO2 levels in both the atmosphere and ocean.[3]

See also[edit]

References[edit]

  1. ^ McCracken, Mark. "Definition of Buffer Factor (Revelle Factor)" (website). Science. Retrieved 2015-11-24. 
  2. ^ a b "7.3.4.2 Carbon Cycle Feedbacks to Changes in Atmospheric Carbon Dioxide" (website). 2010. Retrieved 2015-11-24. 
  3. ^ a b Egleston, Eric; Christopher L. Sabine, Franc ̧ois M. M. Morel (2010). "Revelle Revisited: Buffer Factors That Quantify the Response of Ocean Chemistry to Changes in DIC and Alkalinity" (PDF). Science. 4 (367): 1–9. doi:10.1029/2008GB003407. Retrieved 2015-11-24.  Cite uses deprecated parameter |coauthors= (help)
  4. ^ Sabine, Christopher L.; Richard A. Feely, Nicolas Gruber, Robert M. Key, Kitack Lee, John L. Bullister, Rik Wanninkhof, C.S. Wong, Douglas W.R. Wallace, Bronte Tilbrook, Frank J. Millero, Tsung-Hung Peng, Alexander Kozyr, Tsueno Ono, Aida F. Rios (2004). "The Oceanic Sink for CO2" (PDF). Science. 305 (367): 367–71. doi:10.1126/science.1097403. PMID 15256665. Retrieved 2010-05-19.  Cite uses deprecated parameter |coauthors= (help)