• The average solar power per unit area spread over the whole Earth is

          (Fπr**2)/(4πr**2) = F/4 ≅ 340 W/m**2,

    where F is the solar constant, r is the Earth radius, πr**2 is the cross section of the Earth for catching solar flux, and 4πr**2 is the surface area of the Earth.

  • As the image shows, only about incoming solar flux is absorbed by the ground on average: i.e., ∼ 170 W/m**2.

    Some solar flux is reflected and some is absorbed by the atmosphere.

    Actually, the atmosphere is fairly transparent in the visible band (fiducial range 0.4--0.7 μm) where the solar flux peaks.

  • To digress for a moment, there is a lot of solar flux for abundant solar power in principle since the Earth area. But the energy density per unit time (i.e., power density) is low. Even if you could harvest all of it---and you can only harvest ∼ 10--20 % practically speaking---one square meter would power only about one 150-watt incandescent light bulb.

    The low energy density is the drawback of solar power.

  • Now all the energy from the Sun comes in as relatively low-entropy EMR mostly in the visible band (fiducial range 0.4--0.7 μm).

    By the 2nd law of thermodynamics, the entropy of the energy must increase overall if you are NOT in thermodynamic equilibrium in closed system. The Earth is NOT a closed system and NOT in thermodynamic equilibrium.

    However, entropy in increasing overall, it create even lower-entropy (i.e., more highly ordered) structures: climate, weather, and the biosphere.

    Complex interactions allow this.

    The structures are NOT only ordered, but very complex---which is a different thing from ordered in physics.

    Every bit of energy from the Sun leaves the Earth.

    That part which isn't just reflected leaves as relatively high-entropy EMR mostly infrared.

  • How does the solar flux set the average temperature of the Earth's surface and Earth's atmosphere?

    The solar flux has a nearly blackbody spectrum since the Sun approximates a blackbody radiator.

    However, the solar flux is reduced in energy by spreading out from the Sun and CANNOT heat an absorbing surface to the photospheric temperature of the Sun which ∼ 5800 K.

    As a first approximation, let's say that the Earth absorbs all solar flux and comes to a single temperature. Then the Earth would radiate exactly like blackbody radiator. Using conservation of energy and the Stefan-Boltzmann law we could calculate its single temperature.

    If we did the calculation (which we won't), we would get ∼ 5° C (278 K) (see Wikipedia: Greenhouse effect).

    A slight variation is to say that the Earth absorbs only the solar flux allowed by its actual albedo (diffuse reflectivity). The Earth Bond albedo (overall Earth albedo) is 0.306, and so the absorption fraction is 0.694.

    In this case, we get ∼ -18° C (255 K). (see Wikipedia: Greenhouse effect). This value is probably more suggestive of the true temperature of an real airless Earth since an absolutely zero-albedo airless Earth is unlikely.

  • The actual average temperature of the Earth's surface (we are NOT considering up in the atmosphere nor below the ocean is currently ∼ 15° C (288 K) (see Wikipedia: Instrumental temperature record: Absolute temperatures v. anomalies).

    To 1st-order, the blackbody-radiator Earth approximations to surface temperatures were NOT bad. On the Kelvin scale, the first is only ∼ 3 % too low and the second is only ∼ 10 % too low.

    However, from the perspective of life, the approximate values are significantly low: i.e., chilly.

  • Why is the actual average surface temperatures significantly higher than the values obtained assuming a blackbody-radiator Earth?

    Well the Earth (now counting the atmosphere) is NOT at a single temperature.

    There is temperature gradient that decreases going upward from the Earth's surface.

    The surface temperature will arrange itself so that given the solar flux inflow to the surface (≅ 170 W/m**2) and the opacity (effectively thermal insulation in homey terms) of the atmosphere, the outflow of EMR to space exactly balances the inflow.

    The important opacity (which is mainly in the infrared) is due mainly to water vapor and secondarily to carbon dioxide (CO_2). There are a few minor helpers (e.g., methane (CH_4)).

    If the inflow and outflow of flux are out of balance, then the surface temperature adjust to bring them into balance.

    For example, if you increase the opacity, the outflow falls, the surface temperature increases, the temperature gradient to space steepens (i.e., decreases more rapidly), and the outflow rises again to restore the balance.

    Note Heat flow increases with steepening temperature gradient as a general rule.

    Really, the situation is like heating a house. All the heat flow from a furnace must flow to the outside no matter what. But by increasing the thermal insulation, the inside temperature must rise to maintain the balance of inflow and outflow.

  • We call the insulating effect of the atmosphere the greenhouse effect.

    The greenhouse effect is good.

    It keeps the average surface temperature well above the chilly temperatures that a blackbody-radiator Earth would give.

    But we want the right amount of greenhouse effect which is the amount the biosphere is used to having since ∼ 9000 BCE (i.e., since almost the beginning of Neolithic (c.10,000--c.4500+ BCE) and Holocene (c.10,000 BCE--present) (see Wikipedia: Keeling curve: Mauna Loa measurements).

    But humankind has been increasing the atmospheric carbon dioxide (CO_2) since the Industrial Revolution (c.1750) and very rapidly since circa 1960 (see NOAA: Trends in Atmospheric Carbon Dioxide; Wikipedia: Keeling curve: Mauna Loa measurements), and so increasing the greenhouse effect and the average surface temperature.

    The increasing average surface temperature could have disastrous effects for the biosphere and humankind.

  • By the by, the greenhouse effect is a misnomer for ordinary greenhouses. The inside heat caused by sunlight CANNOT escape easily NOT primarily because glass (i.e., silicate glass) is opaque to infrared (fiducial range 0.7 μm -- 0.1 cm) beyond ∼ 4 μm (see Wikipedia: Glass: Optical properties), but because convection is prevented by the enclosure of the greenhouse. A closed shed heats up pretty much the same even though NO sunlight gets in. See Wikipedia: Greenhouse effect: Real_greenhouses.

  • There are actually two other heat flows to the Earth's surface which are much less important than the solar flux as heat flows, but are very important in other senses:

    1. The geothermal heat flow of from the Earth's interior is on average 0.087 W/m**2 (see Wikipedia: Geothermal gradient: Heat flow). Clearly this is virtually insignificant compared to the solar flux to the Earth's surface of ∼ 170 W/m**2 as a heat flow.

      The energy that powers climate, weather, and the biosphere comes almost entirely from solar flux.

      There is some locally significant contributions of geothermal heat flow at points where it is concentrated: e.g., hydrothermal vents, hot springs, and volcanoes.

      The deep biosphere (deep subterranean life) obviously depends on geothermal heat flow or it would be too cold for life as we know it.

      But we don't worry much about the deep biosphere.

      Of course, geothermal heat flow is NOT negligible even if contributes little directly to climate, weather, and the biosphere.

      It creates geological structures: e.g., plate tectonics, volcanoes, mountain formation, etc.

      Some of geothermal heat flow becomes macroscopic forms of energy to create the structures before being dissipated back to heat energy.

    2. The tidal heat flow whose heat energy ultimately comes from the macrosopic rotational and orbital energy of the Earth, Moon, and Sun.

      The energy is transferred to the tital motional on Earth, both as the macroscopic energy of sea tides and land tides.

      Viscosity and friction turn the energy into heat energy rather rapidly.

      The total tidal heat flow is ∼ 0.0074 W/m**2.

      The tidal heat flow is about a tenth of geothermal heat flow, and so is mostly insignificant in direct contributions to climate, weather, and the biosphere.

      However, the macroscopic energy of the tides which does have an effect coasts, ocean currents, ocean flows in general, weather, and the biosphere.