When can surface temperature be more important than air temperature in dew formation on grass?
Dew forms on surfaces so local surface cooling can be decisive. Exam tip: understand surface-air temperature difference.
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Dew forms on surfaces so local surface cooling can be decisive. Exam tip: understand surface-air temperature difference.
View question detailsEvaporation is a surface process so larger area can raise potential rate. Exam tip: remember the term surface process.
View question detailsWarm air has higher saturation capacity so the same vapour gives a lower percentage. Exam tip: observe daily temperature change.
View question detailsHigh relative humidity weakens the body's natural cooling process. Exam tip: connect sensation with evaporation.
View question detailsEnergy is released when vapour becomes liquid and absorbed when liquid becomes vapour. Exam tip: remember energy direction in phase change.
View question detailsLow humidity and heat together increase evaporative demand. Exam tip: connect soil moisture with weather factors.
View question detailsRelative humidity includes capacity which changes with temperature. Exam tip: understand relative as a ratio.
View question detailsVertical motion causes adiabatic cooling and moisture may condense. Exam tip: remember uplift and cooling together.
View question detailsA cold surface provides contact cooling and vapour can become visible droplets. Exam tip: identify cold-surface condensation.
View question detailsMoisture amount and temperature together decide the state of air. Exam tip: treat the three processes as distinct but connected.
View question detailsA small difference shows little evaporation at the wet bulb and already moist air. Exam tip: link psychrometer reading with relative humidity.
View question detailsLarge wet-bulb depression means evaporation caused more cooling and the air is relatively dry. Exam tip: use dry-bulb and wet-bulb difference as a humidity indicator.
View question detailsMixing creates a new balance between dew point and temperature. Exam tip: treat mixing fog as a special saturation case.
View question detailsCondensation releases heat so saturated rising air cools more slowly. Exam tip: use this as the reason for dry and moist lapse rates.
View question detailsHigh dew point means high actual moisture in air. Exam tip: remember the temperature dependence of (RH).
View question detailsEvaporation needs both humidity deficit and energy. Exam tip: identify energy-limited evaporation separately.
View question detailsMore moisture can reduce the temperature-dew point spread. Exam tip: connect cloud base with dew point spread.
View question detailsCold air trapped in a valley can reach dew point. Exam tip: link valley fog with inversion and moisture.
View question detailsSalinity can slightly lower vapour pressure and affect evaporation. Exam tip: treat it as a secondary factor.
View question detailsWhen the same moisture spreads over many particles, droplets may stay small. Exam tip: remember the link between nuclei number and droplet size.
View question detailsQUIZ COMPLETE