User Tools

Site Tools


nyrad35

Differences

This shows you the differences between two versions of the page.

Link to this comparison view

Both sides previous revisionPrevious revision
Next revision
Previous revision
nyrad35 [2026/06/01 09:38] kerstinnyrad35 [2026/06/01 09:41] (current) kerstin
Line 8: Line 8:
  
 ===== Principle ===== ===== Principle =====
-The NYRAD35 is a dual-polarization simultaneous transmission and simultaneous reception (STSR; also referred to as hybrid-mode, or STAR, simultaneous transmission and reception) radar, with elevation-scanning capabilities. The scanner can perform full 180° scans in elevation and is operated at a constant azimuth of approximately 27°, i.e., along the north-north-east to south-south-west direction. STSR radars receive at horizontal and vertical polarization but transmit a signal that is linearly polarized at 45° direction between vertical and horizontal directions. This allows both for linear depolarization ratio (LDR) observations in zenith and typical dual-polarization variable observations at low elevations, such as differential reflectivity (ZDR) or specific differential phase (KDP). Matching Ka- and W-band observations at zenith allows calculation of the DWR to obtain information on the characteristic size of the ice particle population.+The NYRAD35 is a dual-polarization simultaneous transmission and simultaneous reception (STSR; also referred to as hybrid-mode, or STAR, simultaneous transmission and reception) radar, with elevation-scanning capabilities. The scanner can perform full 180° scans in elevation and is operated at a constant azimuth of approximately 27°, i.e., along the north-north-east to south-south-west direction. STSR radars receive at both horizontal and vertical polarization but transmit a linearly polarized signal at 45° (between the vertical and horizontal polarization planes). This allows both for linear depolarization ratio (LDR) observations in zenith and typical dual-polarization variable observations at low elevations, such as differential reflectivity (ZDR) or specific differential phase (KDP). Matching Ka- and W-band observations at zenith allows calculation of the DWR, providing information on the characteristic size of the ice particle population.
  
  
Line 46: Line 46:
 | Weight | Radar main body: 160 kg, Table: 35 kg, Blower: 109 kg |  | | Weight | Radar main body: 160 kg, Table: 35 kg, Blower: 109 kg |  |
 | Maximum Power Consumption | Radar: max. 1100 W, Blower: 850 W, Scanner: 800 W, 230 V AC, 50-60 Hz |  | | Maximum Power Consumption | Radar: max. 1100 W, Blower: 850 W, Scanner: 800 W, 230 V AC, 50-60 Hz |  |
-| Elevation Scanning | zenith mode, 30° elevation mode | azimuth direction fixed to 27° (along north-north-east to south-south-west direction); elevation angle adjustable; alternating continuous zenith/low-elevation measurements |+| Elevation Scanning | zenith mode, 30° low-elevation mode | azimuth direction fixed to 27° (along north-north-east to south-south-west direction); elevation angle adjustable; alternating continuous zenith/low-elevation measurements with 1°/sec elevation scan  in-between |
 | Manufacturer | [[http://www.radiometer-physics.de/|RPG]] |  | Manufacturer | [[http://www.radiometer-physics.de/|RPG]] | 
  
nyrad35.1780306697.txt.gz · Last modified: 2026/06/01 09:38 by kerstin