Why are leaves green?

“Better a little with tranquility, than an abundance with chasing after the wind”

Thus wrote the ancient scriptural author, whose wisdom encapsulates the answer to the question in the title.

An organism or an organisation needs resources. But securing the resource is just the start – it must then be processed and “harvested”. And if the resource is energy, then too much of it in too short a time, or too much fluctuation of energy input, can reduce efficiency at best and at worst, cause damage. How best to harvest the resource without risking the damage? How to avoid the deadly error of Icarus who flew too close to the sun, overdosing on solar energy?

OK a circuitous route to answering our question but let’s get to it. The photosynthesis of plants and bacteria is one of the most amazing biochemical achievements of the living world, and is the source of most of life’s substance. Early in the evolution of life, organisms learned to harvest light and use it’s power – freely shining down from above – to split water and gain chemical reducing power to build complex organic molecules, cells and multi-celled life forms.

The spectrum of light from the sun – shown above with intensity on the vertical axis, shows that if light were a three course meal, green would be the main course. Green fills the central most intense part of the spectrum. By contrast red and blue at the sides of the visible light spectrum are more like the starter and the dessert: satisfying but less substantial than green.

Most photosynthesising leaves are green. What does this mean in terms of how leaves harvest light? Well it means that they say “no thanks” to the main course abundant green photons in the middle of the spectrum, reflecting them selectively and thus resulting in visible green colour. Instead they absorb and harvest the peripheral colours of red and blue-violet at the fainter extremes of the visible spectrum. It is these edge-of-spectrum coloured photons that are harvested for life-building energy by plant photosynthesis.

Superficially this might seem surprising. Why not absorb the most abundant green photons? Why not have blue or purple leaves? Or red? The answer to this question is a very interesting and counter-intuitive one, but once we see the reason, we will find it to contain a deep lesson of wisdom and the inspiring intelligence of nature. That trying to grab too much can be counter-productive.

The answer to our question “why are leaves green” is presented in the 2020 Science journal entitled “Quieting a noisy antenna …” by Trevor Arp and colleagues – here’s the paper:


Essentially, it’s about stability. Smoothness and stability of the supply of photosynthesis energy from the power source – light – that can be highly variable and unstable. The authors describe the complex biochemical network of light harvesting cell machinery as an “antenna”. This turns quantum photon energy of light into chemically available energy in a series of steps. The antenna is very efficient, but also sensitive. If the incoming light flux were to suddenly become too intense, the network could be damaged by photo-oxidation. So how to safely and efficiently harvest a highly variable intake of light is a difficult challenge.

It turns out that rejecting green photons of the spectrum center and absorbing less abundant red and blue-purple photons provides a solution to this challenge. Why it does so does not have an easy or short explanation. But it has been nicely illucidated by the study by Arp and colleagues.

Think of a leaf in a forest. Let’s say a small or medium shrub or tree with some leafy canopy above it from taller trees. The wind blows, the branches sway, and the mottled light penetrating the canopy to our leaf can vary widely in intensity. For a lot of the time only faint diffuse light reaches the leaf. But now and again for brief moments, the leaf gets a ray of pure sunlight directly, lighting it up suddenly with the full direct light of the sun. The “goal” of the leaf is to provide for the tree a more or less steady supply of chemical energy from sunlight. It turns out that one strategy that succeeds in efficiently harvesting light while also stabilising both the input and output of light energy, is the spectral selection strategy of being green – rejecting the peak green photons and gobbling up instead the edge-of-spectrum red and blue-violet.

Fig. 4 from the paper: Predicted absorption spectra of a finely tuned noisy antenna under seawater.

To show this the authors used computer simulation. They simulated the whole scenario – highly variable full-spectrum light input into an antenna comprising the light harvesting network, and looked for strategies to get stable, efficient output while at the same time avoiding harmful photo-oxidation from over-intense light. Remarkably, their simulations produced absorption spectra that were strikingly similar to the actual absorption spectra of leaves. Or bacteria – which also photosynthesise, being the first organisms to do so 3 odd billion years ago. (And yes – eukaryotic photosynthesis may also still be bacterial in a sense since the intercellular chloroplasts are descended from microbial endosymbionts.) Trevor Arp and colleagues looked at plant and bacterial photosynthesis in a range of scenarios on land and in the sea. The optimised absorption spectra that their simulations produced for harvesting light safely and efficiently, matched closely what they found. This held true for the class of photosynthetic bacteria that are purple as well.

Here’s the abstract of the paper:

Photosynthesis achieves near unity light-harvesting quantum efficiency yet it remains unknown whether there exists a fundamental organizing principle giving rise to robust light harvesting in the presence of dynamic light conditions and noisy physiological environments. Here, we present a noise-canceling network model that relates noisy physiological conditions, power conversion efficiency, and the resulting absorption spectra of photosynthetic organisms. Using light conditions in full solar exposure, light filtered by oxygenic phototrophs, and light filtered under seawater, we derived optimal absorption characteristics for efficient solar power conversion. We show how light-harvesting antennae can be tuned to maximize power conversion efficiency by minimizing excitation noise, thus providing a unified theoretical basis for the observed wavelength dependence of absorption in green plants, purple bacteria, and green sulfur bacteria.

8 responses to “Why are leaves green?”

  1. Most illuminating. Thank you very much.
    Observation. Grape vine leaves and fruit, are affected by short wave spectra. White fruit exposed to the sun lose their chlorophyll relatively early and taste less ‘green’ as a result. Shielded by leaves, the pressed juice is green, with apparently plenty of chlorophyll. The green flavor is most concentrated near the seeds in the middle of the berry and least near the skins. The skins of more sun exposed fruit goes golden yellow with little brown spots like freckles on human skin. Reds become darker if light exposed and stay pink and more transparent in the shade and retain their chlorophyll.
    Skin damage in reds due to overexposure to light, in the Southern Hemisphere where the UV spectrum is stronger due to less ozone aloft, offers an entry to botrytis that results in ‘slipskin’ where the skin readily detaches from the pulp. This fruit yields more colour as its pressed before fermentation. Of course the flavor also changes and not to the good. So, the development of colour in reds is favoured by exposure to more light but too much is a disadvantage.

    When volcanoes send chemicals into the stratosphere ozone is depleted. The upper troposphere at Jet stream levels, 250 hPa cools due to reduced ozone heating. Ice cloud forms and the Earth can be two degrees Celsius cooler for a couple of years. This informs us as to the importance of cloud that reflects about thirty percent of solar radiation back to space. That’s the average. Least in August, most in December when solar radiation is 6% stronger due to orbital distance. NASA Ceres program has measured albedo since 2000. When albedo falls in December, the southern Ocean at latitude 20-40 South warms at the surface. Shallow water warms strongly, deep water hardly at all.

    The Southern Hemisphere absorbs more energy than it emits in long wave radiation. In the Northern Hemisphere that relationship is reversed.

    Liked by 1 person

    1. Thanks Erl for that illuminating comment! So do some green grape varieties require some sun shielding to get the desired grape and wine quality?

      Regarding the hemispheres and radiation budget, there is signify”heat piracy” (love the term!) flowing from SH to NH in the equatorial Atlantic – a consequence of the AMOC. Does this balance out the radiation budget? Or are they unrelated?


      1. I prefer the grapes to ripen in the sun. Wine can taste hard if it has too much acid or too much green flavor. In my experience if the leaves are on the turn from green to autumn colours the berries should be golden rather than green. But if you irrigate and fertilize that result is unlikely. Better to keep a mulch on the soil and make sure moisture is conserved that way.

        That heat piracy is even stronger in the Pacific because the equatorial currents are diverted North by all the Islands of South East Asia and the Pacific Ocean is a lot wider than the Atlantic. But the shape of the South American continent ensures that all the tropical warmth is diverted north. I guess some of the Pacific warmth gets through the Sunda Straits and the gaps between the Islands to warm the Indian Ocean.

        Interestingly, the steepest temperature increase during a warming period in the southern hemisphere is between 30 and 40° south latitude. That zone is now cooling fast. The big rain has come.

        The temperature data indicates warming in all months in the Northern Hemisphere of about a third more than the warming in winter in the Southern Hemisphere. The temperature of the Southern Hemisphere has not advanced in December and January for three decades.

        So, no carbon signal in the lowest common denominator. It’s a complete furphy.

        Liked by 1 person

      2. I guess grape vines need dry conditions but not too dry. Can’t speak from experience. Winemaking must require several areas of knowledge – geology, meteorology and the vine culture, no doubt others.

        Heat piracy is most often discussed in the meridionally bounded Atlantic, but it makes sense that the Pacific should also play a role. Again it’s land configuration that causes this. It’s astonishing that in current literature about palaeo climate when “explaining” climate changes tectonic land rearrangement is ignored and only CO2, silicate weathering etc. are mentioned. (Even mountain uplift is also ignored e.g. Himalayas.) As a result the research effort is essential wasted and the search for truth about the past misdirected. The carbon religion brings much money into climate research but not much new knowledge.


      3. I have read that before the Drake Passage opened between Antarctica and South America the equator to pole temperature gradient was not as steep as today.

        Liked by 1 person

      4. Indeed not – it was the cutting off of the Southern continent and establishment of the globe-ringing southern ocean current that stopped previous supply of warm water from Africa and essentially pushed the earth into its current – and possibly still deepening – glaciation. Antarctica is not getting any warmer – I’ve got a few psts on the subject. I have a hunch that Antarctica is the most important place regarding global climate.


  2. Thanks for the comment Phil,
    Chapter 4 in my book bears on this question . It downloadable here:https://cdn.shopify.com/s/files/1/1628/1053/files/The_Movement_of_the_Atmosphere.pdf?v=1635129636
    Latitudes beyond about 35° North and South are a bottomless sink for energy. Temperature in these mid to high latitudes is a product of transfers from the warmer zone where energy gained via insolation exceeds that lost to radiation. The Northern Hemisphere benefits from energy gained in the Southern, the energy transported by the winds, the currents and as water vapour.
    The Southern Hemisphere is ocean dominant. Water is transparent, absorbing and storing energy in a way that land masses cannot. The flux in cloud cover in southern summer drives variations in the energy incident at the surface. The global atmosphere is coolest in December due to low rates of atmospheric heating because the land masses are coldest at this time. So global cloud cover peaks in December-February when insolation from the sun also peaks due to orbital proximity. Average global temperature is lowest in December, highest in July.
    Variations in albedo when the Earth is closest to the sun determines the flux of incident energy at the surface over the Oceans which have the ability to store and transport that energy, a natural battery.
    To first order global albedo depends on the distribution of the land masses. Secondly, it depends on the extent of atmospheric heating in the cloud bearing layers by ozone.
    The atmosphere doesn’t respect classical notions of an overturning troposphere and a stably stratified stratosphere.
    Polar atmospheric processes, primarily over Antarctica drive ozone variability. The ‘climate shift’ of 1976-8 was a product of a steep increase in the temperature of the global stratosphere as the intake of nitrogen oxides of mesospheric origin effectively stalled. But, the southern stratosphere has been cooling slowly since that time and, if this continues there will be a return to the cool conditions of the 1960s-70s when people worried about the globe icing up.

    Liked by 1 person

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