MLchartDataset catalogue

Wet growth

Term · Meteorology and atmospheric science · MLC-T-MET-010214

The process by which ice particles, such as hail or graupel, grow by collecting supercooled liquid water droplets that freeze upon impact. This occurs when the ice particle's surface temperature is near 0 degrees Celsius, allowing some of the collected water to spread before freezing. It leads to the formation of clear ice layers within hailstones.

Table 1. Record
IdentifierMLC-T-MET-010214
FieldMeteorology and atmospheric science
See alsoDry growth
Record as JSON
{
  "id": "MLC-T-MET-010214",
  "term": "Wet growth",
  "field": "Meteorology and atmospheric science",
  "definition": "The process by which ice particles, such as hail or graupel, grow by collecting supercooled liquid water droplets that freeze upon impact. This occurs when the ice particle's surface temperature is near 0 degrees Celsius, allowing some of the collected water to spread before freezing. It leads to the formation of clear ice layers within hailstones.",
  "see_also": [
    "dry growth"
  ],
  "url": "https://mlchart.com/terminology/meteorology/wet-growth/"
}

Record 10,583 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.