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Warner L. Ecklund

Researcher at Cooperative Institute for Research in Environmental Sciences

Publications -  97
Citations -  4657

Warner L. Ecklund is an academic researcher from Cooperative Institute for Research in Environmental Sciences. The author has contributed to research in topics: Radar & Wind profiler. The author has an hindex of 39, co-authored 97 publications receiving 4525 citations. Previous affiliations of Warner L. Ecklund include University of Colorado Boulder & National Oceanic and Atmospheric Administration.

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Long‐term observations of the Arctic mesosphere with the MST radar at Poker Flat, Alaska

TL;DR: In this article, the authors summarize the results of 22 months of observations of Arctic mesosphere echoes with the 50-MHz radar at Poker Flat, Alaska and conclude that during summer months the mesospheric echoes are relatively continuous in time and extend from about 80 to 100 km with an unexpectedly strong peak in signal-to-noise ratio at about 85 km.
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Developments in UHF lower tropospheric wind profiling at NOAA's Aeronomy Laboratory

TL;DR: An overview of the architecture of the UHF profiler system as it has evolved over the past decade including the development of radio acoustic sounding system (RASS) capabilities is presented in this paper.
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Classification of Precipitating Clouds in the Tropics Using 915-MHz Wind Profilers

TL;DR: In this paper, an algorithm was developed that classifies precipitating clouds into either stratiform, mixed stratiform/convective, deep convective, or shallow convective clouds by analyzing the vertical structure of reflectivity, velocity, and spectral width derived from measurements made with the vertical beam of a 915-MHz Doppler wind profiler.
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A UHF Wind Profiler for the Boundary Layer: Brief Description and Initial Results

TL;DR: In this paper, a boundary layer radar was developed at NOAA's Aeronomy Laboratory for use in a hybrid mode with existing 50 MHz profilers in the tropical Pacific, and the system can equally be a stand-alone device to study boundary layer problems.
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Evidence for a Rayleigh-Taylor type instability and upwelling of depleted density regions during equatorial spread F

TL;DR: In this article, a Rayleigh-Taylor gravitational instability operating on the bottom side of the F peak is explained for strong radar echoes typically observed in patch-like structures at high altitudes.