Learn what bombogenesis measures, why the pressure threshold changes with latitude, where bomb cyclones form and which local forecasts matter most.
Tornadoes can follow several storm-scale pathways. Learn what supercells and downdrafts contribute, what radar confirms, and how to shelter safely.
How thunderstorms grow, why lightning and hail develop, how to read a storm forecast, and what to do as soon as thunder is heard.
Relative humidity depends on temperature. Dew point tracks the moisture itself, and an outdoor humidity forecast does not describe indoor air.
How observations, MOR, kilometres and statute miles differ, why fog is below 1 kilometre, and how to read a visibility forecast.
How observations, data assimilation, models, ensembles, and calibration become a weather forecast, and why the result changes with lead time.
Cloud-cover percentages and oktas describe sky amount, not rain chance or height. Layers overlap, and a ceiling is a separate aviation report.
How Airpult calculates sunrise, sunset and day length, why visible times can differ, and how twilight, latitude and local time affect the result.
Understand mean wind, gusts, measurement height, forecast periods, the Beaufort scale, and practical decisions in exposed conditions.
How Airpult calculates Feels Like temperature, why provider values differ, and how wind, humidity, sun, clothing and activity affect your experience.
How Airpult combines six CAMS pollen forecasts into tree, grass and weed groups, what the display levels mean, and how weather can change airborne pollen.
What AQI means, why US and European readings differ, and how Airpult’s model-derived value compares with official reporting.