
Severe Weather 101: Hail Basics - NOAA National Severe Storms …
Hail is a form of precipitation consisting of solid ice that forms inside thunderstorm updrafts. Hail can damage aircraft, homes and cars, and can be deadly to livestock and people. What we do: …
Severe Weather 101: Hail Types - NOAA National Severe Storms …
NSSL's Hydrometeor Classification Algorithm, or HCA, uses dual-polarization technology to automatically sort between ten types of radar echoes including big raindrops and hail. This …
the HSDA to classify the size of the hail into 1 of 3 categories: small (D < 1”), large (1” ≤ D < 2”) or giant (D ≥ 2”). The HSDA only uses 3 dual-pol variables and their associated quality fields:
Severe Weather 101: Thunderstorm Types - NOAA National Severe …
Often called “popcorn” convection, single-cell thunderstorms are small, brief, weak storms that grow and die within an hour or so. They are typically driven by heating on a summer afternoon. …
the hail of small and giant sizes are much more pronounced than the corresponding differences in Z. The plots in Fig. 3 were used to specify parameters of the membership functions in different …
Severe Weather 101: Hail Detection - NOAA National Severe …
Hail Detection. Hail can be detected using radar. On Doppler radar, hail generally sends a return signal that looks like extremely heavy rainfall. Dual-polarization radar technology, used by the …
Severe Weather 101: Hail Forecasting - NOAA National Severe …
Information about hail forecasting, models and methodology, from the NOAA National Severe Storms Laboratory.
Severe Weather 101: Lightning Basics - NOAA National Severe …
Scientists think that the initial process for creating charge regions in thunderstorms involves small hail particles called graupel that are roughly one quarter millimeter to a few millimeters in …
NSSL Projects: mPING Weather Types Explained
Hail: A chunk of ice falling from the sky ranging from the size of a pea to a grapefruit; hail occurs exclusively in thunderstorms. Sleet is not tiny hail but is instead produced by a different process.
Because most convective storms produce small hail, at least aloft, routine observations of the polarimetric TBSS at C band would indicate that these small stones produce enough of a …