A full spectrum of colour- based descriptions has emerged to describe the properties and
distribution of organic carbon: black, brown, red, blue, green and teal. This colour- based terminology contributes to our evolving understanding of the carbon cycle by moving past traditional, broad classifications of carbon types (often as simple as inorganic vs. organic carbon), to more nuanced definitions based
on carbon function, attribute, or location. For example, some of the colours (blue, green and teal) highlight the role of carbon in climate change mitigation via sequestration. Other types (black, brown and red) impact Earth’s heat balance or promote cryospheric melting.

Red carbon is the newest colour in the carbon spectrum. “In its broadest context, it includes
all living biological particles on snow and ice that reduce albedo to survive” describes Roman Dial, Professor at Alaska Pacific
University, USA (Dial, R. J. et al. FEMS Microbiol. Ecol. 94, fiy007; 2018). Red expresses a common
pigment produced by snow microorganisms, but the term also encompasses pigments spanning yellow through to purple.
These colours absorb abundant green and blue wavelengths of light, melting the snow and ice, and “producing liquid water necessary
for life, and freeing up nutrients (such as nitrogen and phosphorous) that are bound
within ice crystals” adds Dial. Although the red carbon moniker has not yet caught on, the impact of reduced albedo from the
pigments is known to increase snow melt, as seen in the Arctic (Lutz, S. et al. Nat Commun. 7, 11968; 2016), motivating increasing research into the role of microorganisms and the cryosphere.

Black carbon, one of the best known colours of carbon, also reduces snow and ice albedo
thus increasing melting, and along with brown carbon, is produced through the incomplete
combustion of organic matter.

Some of the production is natural (such as during wildfires) but fossil fuel burning and industrial activities
are also major sources (Bond, T. C. et al. J. Geophys. Res. Atmos. 118, 5380–5552; 2013).

In comparison with black carbon, which is often described as graphitic and absorbing a wide
spectrum of light, brown carbon is the visible and UV- light- absorbing component of organic aerosols. However, both of these terms change with advancing technologies. For instance, black carbon was initially identified visually, but now Ellen Druffel, Professor at University of California Irvine, USA, notes there is a spectrum from “Char produced by partially burning biomass, and soot by the burning of fossil fuels.”

Similarly, a multitude of organic compounds, including some that are produced by secondary processes in the atmosphere, have been identified within the umbrella term brown carbon (Laskin, A. et al. Chem. Rev. 115, 4335–4382; 2015). What is clear for both carbon
types is that in addition to reducing air quality, they absorb solar radiation at the top of the
atmosphere, retaining heat and impacting climate. Yet, recent “interest in using biochar as a way to store carbon”, as stated by Druffel, has led to broader research of black carbon for climate change mitigation, casting this dark
carbon in a more positive light.

Carbon sequestration has also sparked interest in green, blue and teal carbon. These colours are united by describing the location
of the carbon, rather than an inherent physical property.

Green carbon reflects “the carbon
sequestered by land ecosystems” states Carlos Duarte, Professor at the King Abdullah University of Science and Technology, Saudi Arabia, and incorporates carbon in soils and within biomass such as forests.