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DOPPLER RADAR OAHU ARCHIVE
DOPPLER RADAR OAHU PLUS

Our team of meteorologists dives deep into the science of weather and breaks down timely weather data and information. It worked out then and has done so throughout his impressive career. The headwinds the Project NIMROD team faced in the 1970s showed Wakimoto the importance of sticking to what you believe in when you have evidence backing you up. He acknowledges it takes time and commitment and adds he’s working to partner with a historically Black college/university and is excited about the possibilities that may bring. Increasing diversity is also one of his priorities. Wakimoto has seen the value of bridging research across disciplines when returned to UCLA, he added the “creative activities” part to his job title. “I don’t take these responsibilities lightly, so I always endeavor to make choices that I believe will benefit the entire community,” he says. He also spent time as a leader at both the National Science Foundation and National Center for Atmospheric Research.Īt UCLA, he has influence over policies and priorities that affect thousands of students.

Bright reflectivity returns that are stationary and appear during both calm and inclement weather are usually land-based obstructions such as mountains, trees, or especially wind farms (nothing gets electromagnetic signals confused like spinning metal blades!).Wakimoto is now the Vice Chancellor for Research and Creative Activities at UCLA, returning to the university where he taught from 1983 to 2005.

This is helpful for picking out snow/mix/rain transition zones In all snow situations, dBZ values of 40 indicate 3-4”/hr snowfall rates and whiteout conditions. Anything larger than this is usually due to “bright banding” where the radar is seeing the part of the atmosphere where snowflakes are clumping together and melting into raindrops.

In cold climates during the winter months, actual dBZ values rarely exceed 40.

This is your standard radar data that shows precip or other solid/liquid particles in the atmosphere. The first type of data currently available is reflectivity. We currently have two types of radar data available with plans to add more soon. Use radar data with caution especially if your area of interest is far from the nearest radar location! A lot can happen between 0 and 5,000 feet and therefore the depiction of precipitation given by radar may differ some from what’s actually happening on the ground. Because of this phenomenon, the radar beam will only see precipitation falling through the mid levels of the atmosphere. To see this in action, imagine a circle (earth) with a straight line emanating from some point on the circle if you continue this line out into space, it will gradually get farther and farther from the circle. Because the earth is round and the radar beam is flat, the farther away from the radar tower the beam (energy) travels, the farther removed from the ground becomes. For frequently asked questions about the new radar application please see /radarfaq.

For more information please see SCN 20-85. There is a notable constraint to radar data though. On December 17, 2020, the National Weather Service updated the web application hosted at. This is the highest resolution radar data available which enables you to see features such as sea breeze or outflow boundaries that standard resolution radar entirely misses. This data is gathered from over a hundred radar towers located across the US. Lake Murray, Ardmore OK (WeatherOK, USA).

DOPPLER RADAR OAHU PLUS

Lightning CG worldwide (since 2004) Plus.

DOPPLER RADAR OAHU ARCHIVE

Base reflectivity (with archive since 1991).Radar & Lightning Radar & Lightning Radar.Forecast Ensemble Heatmaps (Up to 7 models, multiple runs, graph up to 46 days) Plus.Forecast Ensemble (Up to 7 models, multiple runs, graph up to 46 days) The starting point for official government weather forecasts, warnings, meteorological products for forecasting the weather, and information about meteorology.Forecast XL (Graph and table up to 10 days - choose your model).14 day forecast (ECMWF-IFS/EPS, graphs with ranges).Kohala isn’t an active volcano, as scientists believe the last eruption took place about 120,000 years ago. It is situated near the oldest volcano in the state at the northern tip of the island. Meteograms (Graph 3-5 days - choose your model) The Next Generation Weather Radar (NEXRAD) system is a network of 160 high-resolution S-band Doppler weather radars jointly operated by the National Weather Service (NWS), the Federal Aviation Administration (FAA), and the U.S. Kohala: The Hawaii doppler radar station at Kohala is another station on the island of Hawaii, located opposite of Hilo’s station.

Weather overview (Next hours and days, 14 day forecast).Europa Finnish HD HARMONIE (3 days) new.

Tropical cyclone tracks (ECMWF/Ensemble).