How the planner estimates light

The Window Light Planner is a physics model, not a measurement. This page lists every step and assumption, so you can judge how far to trust a result.

What it calculates

For each month it takes one representative day and works out the daily light integral (DLI): the photosynthetic light, in mol/m²/day, reaching a leaf that faces the window, at the distance you chose, horizontally centered on the window and level with the sill. It gives a range from a cloudier and a clearer month for the weather setting you pick, with a typical value between them. (Usually the clearer month is brighter; for a north window a hazy sky can give slightly more light, because haze spreads light into the northern sky.)

Step 1: where the sun is

Solar declination, Earth–sun distance and day length come from the FAO-56 equations (eqs. 23–25), every 5 minutes from sunrise to sunset on the month's mean day. The model reproduces FAO-56's worked example 8 (extraterrestrial radiation 32.2 MJ/m²/day at 20°S on 3 September), which is one of the automated tests. Its day lengths match FAO-56's table: about 15.0 hours at 40°N in June and 9.3 hours in December.

Step 2: how much reaches the ground outside

Sunlight above the atmosphere is multiplied by a clearness index, the share that gets through clouds and haze. Without a weather database the planner uses three presets, each a range from a dull month to a bright one:

FAO-56 puts a cloudless day at about 0.75. The light is split into direct beam and diffuse sky light with the Erbs, Klein and Duffie (1982) correlation. As a check, the outdoor totals land inside the published US DLI maps of Korczynski, Logan and Faust (2002): 5 to 10 mol/m²/day across the northern US in December, up to 55 to 60 in the Southwest in summer.

Step 3: through the window

Step 4: energy to plant light

42.9% of solar energy is photosynthetically active radiation (400–700 nm), and each joule of it carries 4.57 µmol of photons (Thimijan and Heins, 1983). Together that is 1.96 mol of PAR photons per MJ of sunlight, the conversion used for the US DLI maps.

Step 5: matching plants

Every plant in the database has an ideal light category and the lowest category it copes with, taken from extension services, the RHS or the Missouri Botanical Garden (each plant page lists its sources). The categories are turned into DLI like this:

CategoryGrows well fromHolds on down to
Low light3 mol/m²/day0.54 mol/m²/day
Medium light6 mol/m²/day1.08 mol/m²/day
Bright indirect10 mol/m²/day2.15 mol/m²/day
Direct sun12 mol/m²/day10.75 mol/m²/day

What it does not know

The model makes no claims beyond these steps. Every equation is in the site's source code, with unit tests that check it against FAO-56 and the closed-form geometry.

Sources

  1. Allen, R.G., Pereira, L.S., Raes, D. & Smith, M. (1998). Crop evapotranspiration. FAO Irrigation and Drainage Paper 56, chapter 3
  2. FAO-56 Annex 2, Table 2.7: mean daylight hours
  3. Thimijan, R.W. & Heins, R.D. (1983). Photometric, radiometric, and quantum light units of measure. HortScience 18(6):818-822
  4. Korczynski, P.C., Logan, J. & Faust, J.E. (2002). Mapping monthly distribution of daily light integrals across the contiguous United States. HortTechnology 12(1):12-16
  5. Erbs, D.G., Klein, S.A. & Duffie, J.A. (1982). Estimation of the diffuse radiation fraction for hourly, daily and monthly-average global radiation. Solar Energy 28(4):293-302
  6. pvlib python: isotropic sky and ground-reflected irradiance (Liu and Jordan model) documentation
  7. Howell, J.R. A Catalog of Radiation Heat Transfer Configuration Factors, case B-3
  8. Efficient Windows Collaborative (NFRC consumer guide): window glazing types, visible transmittance
  9. Steil, A. Important considerations for providing supplemental light to indoor plants. Iowa State University Extension
  10. Lighting. Houseplants, University of Illinois Extension
  11. Light for houseplants. UF/IFAS Gardening Solutions
  12. Apogee Instruments: Conversion, PPFD to lux