Skip to contentScholarGate
LibraryBookshelfDeskReview StudioAssistant
Sign in
On this page
IntuitionHow it worksWhen to use itStrengths & limitationsCommon pitfallsApplicationsFrequently asked🔒 Read the full methodSourcesRelated methods
Cite this pageSpotted an issue on this page? Report or suggest a fix →
Home›Meteorology›Lightning Jump
Process / pipelineSevere weather prediction

Lightning Jump

Lightning Jump Severe Weather Indicator · Also known as: Lightning jump, Lightning trend, VHF lightning, Electric field analysis

The lightning jump is a rapid increase in lightning activity (number of flashes per unit time) that precedes severe weather including hail, heavy rain, and tornadoes. This phenomenon, observed using satellite or ground-based lightning detection networks, is an operational diagnostic tool for real-time severe weather warning.

ScholarGate
  1. Process / pipeline
  2. v1
  3. 2 Sources
  4. PUBLISHED
Cite this page →
Tools & resources
Download slides
Learn & explore

Read the full method

Members only

Sign in with a free account to read this section.

Sign in

Method map

The neighbourhood of related methods — select a node to explore.

Lightning Jump
Dual-Polarization RadarWRF Model

When to use it

Use lightning jump as an early indicator of rapidly intensifying convection in real-time warning operations. It is most valuable during rapid convective development when radar-based indicators lag actual intensification. Combine with radar reflectivity, rotation, and wind shear for best results.

Strengths & limitations

Strengths
  • Objective, quantitative criterion; reduces subjectivity in severe weather warning decisions
  • Responds to actual convective intensity, not just size or reflectivity; detects intensification early
  • Available continuously (day and night) from satellite and ground networks; complements radar-based indicators
  • Precedes hail and tornadoes by minutes, providing lead time for warnings
Limitations
  • Lightning jump can occur without severe surface weather in all cases; false alarm rate is not negligible
  • Clouds with suppressed coalescence (e.g., very high aerosol environments) produce less lightning despite intense updrafts
  • Ground-based lightning networks have variable detection efficiency; satellite lightning observations have gaps
  • Relationship between lightning jump and specific severe outcomes (tornado, large hail) is probabilistic, not deterministic

Frequently asked

What defines a lightning jump—is it 50% or some other threshold?

The most common definition is 50% increase in flash count over 60–90 seconds. However, thresholds vary by region and can be tuned based on local climatology and false alarm analysis.

Why does lightning increase just before tornadoes?

Tornadoes occur in environments with strong updrafts and vigorous charge separation. A tornado's parent supercell shows a surge in updraft strength before tornadogenesis; this updraft intensification is marked by increased lightning.

Can we use lightning jump to predict tornadoes with certainty?

No. Lightning jump increases tornado probability but does not guarantee a tornado will occur. Many storms show lightning jumps without producing tornadoes; conversely, some tornadoes occur without a clear lightning jump.

Is satellite lightning data or ground-based data better for lightning jump?

Both have merits. Satellite provides global coverage but with latency. Ground-based networks provide better temporal resolution and detection efficiency for weak lightning. Combining both is optimal.

Sources

  1. Schultz, E., Petersen, W. A., & Rudlosky, S. D. (2009). Preliminary Development and Validation of the Specific Convective Activity Signature (SCAS) Product using Optical Transient Detector and Geostationary Satellite Data. Journal of Applied Meteorology and Climatology, 48(4), 642-655. link ↗
  2. Mosier, R. M., Czarnecki, C., & Carey, L. D. (2011). Radar and Lightning Observations of the 1 August 2008 Kinston, North Carolina Supercell. Weather and Forecasting, 26(4), 459-474. link ↗

How to cite this page

ScholarGate. (2026, June 3). Lightning Jump Severe Weather Indicator. ScholarGate. https://scholargate.app/en/meteorology/lightning-jump

Related methods

Dual-Polarization RadarWRF Model

Which method?

Set this method beside its closest kin and read them side by side — the library lays the books on the table; the choice is yours.

  • Dual-Polarization RadarMeteorology↔ compare
  • WRF ModelMeteorology↔ compare
Compare side by side →

Similar methods

Dual-Polarization RadarVelocity-Azimuth DisplaySkew-T Log-P AnalysisQuasi-Geostrophic Omega EquationSpectral Bin MicrophysicsPotential Vorticity InversionThermal WindWRF Model

Related reference concepts

Thunderstorms and Convective SystemsTornadoes and SupercellsMesoscale and Severe WeatherAtmospheric Stability and ConvectionNowcasting and Statistical ForecastingMeteorology

Spotted an issue on this page? Report or suggest a fix →

ScholarGate — Lightning Jump (Lightning Jump Severe Weather Indicator). Retrieved 2026-07-21 from https://scholargate.app/en/meteorology/lightning-jump · Dataset: https://doi.org/10.5281/zenodo.20539026
Quick facts
Originator
Schultz, Petersen, Rudlosky
Subfamily
Severe weather prediction
Year
2009
Type
Real-time warning product
Related methods
Dual-Polarization RadarWRF Model
ScholarGate

A content-first reference library for research methods — what each one is, how it works, and where it comes from.

Open data (CC-BY)

Explore

  • Library
  • Search the library…
  • Browse by field
  • Fields
  • Journey
  • Compare
  • Which method?

Reference

  • Subjects
  • Atlas
  • Glossary
  • Methodology
  • Philosophy

Your tools

  • Bookshelf
  • Desk
  • Chat

Company

  • About
  • Pricing
  • Contact
  • Suggest a method

Entries are compiled from published sources for reference. Verifying the accuracy and suitability of any information for your own use remains your responsibility.

© 2026 ScholarGate · A research-method reference library
  • Privacy
  • Cookies
  • Terms
  • Delete account