Evaporation and transpiration
How liquid water becomes vapour at Earth's surface, by ocean evaporation and by land transpiration and soil or canopy evaporation, absorbing latent heat and mixing vapour into the lower atmosphere.
Boundary: where this process starts
Starts with: Sunlight heats ocean surface, wet soil and leaves
Boundary: where it ends
Ends after: Water vapour mixes into the lower atmosphere
Line thickness = size of impact (1 to 5)% on a line = chance a fork takes that branch📄 = pieces of evidence on a stepNegative effectLoops backHypothesisResource used up (arrow into the step)Resource used, not used upResource made or released (arrow out of the step)
What am I looking at? The concepts on every map
- Participant
- Someone or something that takes part in a process or influences it: a plant, a microbe, a river, a machine, a force. Participants are the rows of a map.
- Resource
- Something a step uses or uses up: water, oxygen, sunlight, a tool. Each step has an arrow down to the resources it uses.
- Step
- One thing that happens in a process. Every step has at least one participant and carries evidence.
- Decision fork
- A step where the process can go several ways. Every outcome is labeled with a percentage, and the percentages add up to 100%. It is not limited to yes or no.
- Loop
- A line that carries the process back to an earlier step. We record whether it reinforces or balances, how strong it is (weak, moderate, strong), and its gain (0 to 1): the share of the effect that returns on each pass.
- Size of impact
- Every line says how much the earlier step affects the next one (1 to 5), in which direction (+, -, 0), and why. Thicker lines mean bigger impact.
- Evidence
- The support for a claim: a source and what it shows. Every step, line, change and vote needs it. Click any step or line to read its evidence.
- Boundary
- Where a process starts and where it ends. Every process, and every subprocess, has a start and an end.
- Subprocess
- A step that is itself a whole process, with its own boundary, steps and lines. Click a step marked ↘ to open it. Subprocesses nest as deep as the evidence goes.
- Description
- A plain-language summary of what a process is and what it covers.
- Hypothesis
- A proposed new connection between two parts of the map that nobody has linked. It carries a prediction, a way to test it, and a count of papers on each topic and on both. It is an unverified idea until someone tests it.
Every step, with its evidence
The same information as the map, as a list you can search and share. Click a participant or resource to see everywhere it appears.
Sunlight heats ocean surface, wet soil and leaves
Evidence (1) · added by Atlas
- Oki & Kanae 2006, Global hydrological cycles and world water resources, Science 313:1068-1072: Global evaporation ~505,000 km3/yr: ~434,000 from ocean (86%) and ~71,000 from land; precipitation ~398,000 on ocean (78%) and ~111,000 on land (22%); ~40,000 km3/yr flows from land to ocean. (confidence 0.9)
⑂ Source of the water vapour
Evidence (1) · added by Atlas
- Oki & Kanae 2006, Global hydrological cycles and world water resources, Science 313:1068-1072: Global evaporation ~505,000 km3/yr: ~434,000 from ocean (86%) and ~71,000 from land; precipitation ~398,000 on ocean (78%) and ~111,000 on land (22%); ~40,000 km3/yr flows from land to ocean. (confidence 0.9)
Ocean surface water evaporates, absorbing latent heat
Evidence (1) · added by Atlas
- Oki & Kanae 2006, Global hydrological cycles and world water resources, Science 313:1068-1072: Global evaporation ~505,000 km3/yr: ~434,000 from ocean (86%) and ~71,000 from land; precipitation ~398,000 on ocean (78%) and ~111,000 on land (22%); ~40,000 km3/yr flows from land to ocean. (confidence 0.9)
⑂ How land returns water to the air
Evidence (1) · added by Atlas
- Schlesinger & Jasechko 2014, Transpiration in the global water cycle, Agric. Forest Meteorol. 189-190:115-117: Transpiration is about 61% (+/-15) of terrestrial evapotranspiration; the rest is soil, canopy-interception and open-water evaporation. (confidence 0.8)
Roots draw soil water that leaves through leaf pores (transpiration)
Evidence (1) · added by Atlas
- Schlesinger & Jasechko 2014, Transpiration in the global water cycle, Agric. Forest Meteorol. 189-190:115-117: Transpiration is about 61% (+/-15) of terrestrial evapotranspiration; the rest is soil, canopy-interception and open-water evaporation. (confidence 0.8)
Soil, wet canopy and lake surfaces evaporate
Evidence (1) · added by Atlas
- Schlesinger & Jasechko 2014, Transpiration in the global water cycle, Agric. Forest Meteorol. 189-190:115-117: Transpiration is about 61% (+/-15) of terrestrial evapotranspiration; the rest is soil, canopy-interception and open-water evaporation. (confidence 0.8)
Water vapour mixes into the lower atmosphere
Evidence (1) · added by Atlas
- Oki & Kanae 2006, Global hydrological cycles and world water resources, Science 313:1068-1072: Global evaporation ~505,000 km3/yr: ~434,000 from ocean (86%) and ~71,000 from land; precipitation ~398,000 on ocean (78%) and ~111,000 on land (22%); ~40,000 km3/yr flows from land to ocean. (confidence 0.9)