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. There is a notable constraint to radar data though. 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).Lightning CG worldwide (since 2004) Plus.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).Forecast XL (Graph and table up to 10 days - choose your model).14 day forecast (ECMWF-IFS/EPS, graphs with ranges).Meteograms (Graph 3-5 days - choose your model).Weather overview (Next hours and days, 14 day forecast).Central Europe Super HD (MOS) (3 days) new.Tropical cyclone tracks (ECMWF/Ensemble).Harasti,P.R., McAdie,C.J., Dodge, P.P., Lee, W-C, Tuttle, J., Murillo, S.T., Marks, F.D. Rogers, and F.Roux, 2005: “A numerical simulation of Hurricane Bret on 22-23 August 1999 initialized with airborne Doppler radar and dropsonde data” .Soc., 131 (605) p.155-194 (Jan. Zhang, 2010: “Estimation and mapping of hurricane turbulent energy using airborne Doppler measurements.” Monthly Weather Review, 138(9)p.3656-3670 (September 2010) Marks, 2012: “Multiscale analysis of mature tropical cyclone structure from airborne Doppler composites,” Monthly Weather Review, 140 (1), P. Environmental flow impacts on tropical cyclone structure diagnosed from airborne Doppler radar composites. Evaluation of the Hurricane Research Division Doppler radar analysis software using synthetic data. The relationship between spatial variations in the structure of convective bursts and tropical cyclone intensification using airborne Doppler radar. A wavenumber-1 asymmetry arises, showing that in the downshear (upshear) quadrants of the TC, updrafts are more (less) frequent and deeper (shallower)… Rainband updrafts become deeper and stronger with increasing radius. The selected updrafts are then collectively analyzed by their frequency, radius, azimuthal location (relative to the 200–850 hPa environmental wind shear), structural characteristics, and secondary circulation (radial/vertical) flow pattern. An automated algorithm is developed to identify the strongest rainband updrafts across 12 hurricane-strength TCs. Journal of Geophysical Research: Atmospheres, 127(6), e2021JD035718.4Ībstract: Ten years of airborne Doppler radar observations are used to study convective updrafts’ kinematic and reflectivity structures in tropical cyclone (TC) rainbands. Statistical Analysis of Convective Updrafts in Tropical Cyclone Rainbands Observed by Airborne Doppler Radar.
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