Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Daily Arctic Lightning Strokes

Dataset ·
DOI:https://doi.org/10.5439/2377965· OSTI ID:2377965

In recent decades, lightning activity at high latitudes has increased. Tall thunderstorm clouds affect radiation balance directly, as well as indirectly through lightning-initiated fires and the resulting smoke. One can remotely sense lightning strokes over the globe through their VLF radio emission, and, with multiple receivers, it is possible to precisely locate lightning strokes. This technique makes it possible to continuously monitor arctic lightning--a capability not possible by other means. In this research effort, a World-Wide Lightning Location Network station, consisting of a VLF receiver, signal processing hardware, and analysis software, were installed at the North Slope of Alaska (NSA) facility and planned to operate for several years. This far north location is expected to improve the network's high-latitude detection efficiency.

Research Organization:
Atmospheric Radiation Measurement (ARM) Archive, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (US); ARM Data Center, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Contributing Organization:
PNNL, BNL, ANL, ORNL
DOE Contract Number:
AC05-00OR22725
OSTI ID:
2377965
Report Number(s):
ARM0806
Availability:
ORNL
Country of Publication:
United States
Language:
English

Similar Records

Electromagnetic field radiation model for lightning strokes to tall structures
Journal Article · Mon Jul 01 00:00:00 EDT 1996 · IEEE Transactions on Power Delivery · OSTI ID:372254

Search for wave-induced particle precipitation from lightning and transmitter sources. Master's thesis
Technical Report · Thu Dec 31 23:00:00 EST 1987 · OSTI ID:6695152

Some features of stroke occurrence in Florida lightning flashes
Journal Article · Wed Jun 20 00:00:00 EDT 1984 · J. Geophys. Res.; (United States) · OSTI ID:5615638