Differences

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

--- instruments:instruments [2016/10/18 19:25] – [Ceilometer] jan
+++ instruments:instruments [2024/04/16 10:09] (current) – [Cloud Radar] lbuehler
@@ Line 7: / Line 7: @@
 ==== Cloud Radar ====
-Our scanning [[instruments:mira:mira|cloud radar JOYRAD-35]] is a pulsed Doppler radar which measures profiles of reflectivity, Doppler velocity, Doppler spectral width, and linear depolarization ratio at 35.5 GHz. From these, various macro- and microphysical properties of clouds and precipitation can be derived. In addition, we operate the 94 GHz FMCW cloud radar [[instruments:joyrad94:joyrad94| cloud radar JOYRAD-94]] which can resolve cloud structures down to a resolution of 5 m. For background information see the [[http://wiki.eg-climet.org/index.php?title=Cloud_radar|EG-CLIMET wiki]].
+Our scanning [[instruments:mira:mira|cloud radar JOYRAD-35]] is a pulsed Doppler radar which measures profiles of reflectivity, Doppler velocity, Doppler spectral width, and linear depolarization ratio at 35.5 GHz. From these, various macro- and microphysical properties of clouds and precipitation can be derived. For background information see the [[http://cfa.aquila.infn.it/wiki.eg-climet.org/index.php?title=Cloud_radar|EG-CLIMET wiki]]. In addition, we operate the 94 GHz FMCW [[instruments:joyrad94:joyrad94| cloud radar JOYRAD-94]] which can resolve cloud structures down to a resolution of 5 m. The G-band dual-frequency [[instruments:grawac:grawac|cloud radar GRaWAC]] is a FMCW radar at 167.3 and 174.7 GHz with Doppler capabilities. It has a vertical resolution of 30 m and a sensitivity of -43 dBZ at 1 km, 1 s.
 ==== Doppler Lidar ====
-The [[instruments:wind_lidar|Doppler Lidar]] sends out pulses of light in the near-infrared part of the spectrum. The Doppler shift of the signal backscattered by aerosol can be used to infer line-of-sight wind speed within the boundary layer. Scanning in elevation and azimuth allows derivation of the full wind vector. For background information see the [[http://wiki.eg-climet.org/index.php?title=Doppler_Wind_Lidar|EG-CLIMET wiki]].
+The [[instruments:wind_lidar|Doppler Lidar]] sends out pulses of light in the near-infrared part of the spectrum. The Doppler shift of the signal backscattered by aerosol can be used to infer line-of-sight wind speed within the boundary layer. Scanning in elevation and azimuth allows derivation of the full wind vector. For background information see the [[http://cfa.aquila.infn.it/wiki.eg-climet.org/index.php5/Doppler_Wind_Lidar|EG-CLIMET wiki]].
 ==== Meteorological tower ====
@@ Line 20: / Line 19: @@
     * [[instruments:snohat:snohat|HATPRO-SNOHAT]]
     * [[instruments:tophat:tophat|HATPRO-TOPHAT]]
-Additionally, a [[instruments:dpr:dpr|Dual Polarization Radiometer (DPR)]] is operated which measures in mm wavelength atmospheric windows and is highly sensitive to snowfall and super-cooled liquid water. Click [[instruments:mwr_references|here]] for a list of relevant references. For background information see the [[http://wiki.eg-climet.org/index.php?title=Microwave_radiometer|EG-CLIMET wiki]].
+Additionally, a [[instruments:dpr:dpr|Dual Polarization Radiometer (DPR)]] is operated which measures in mm wavelength atmospheric windows and is highly sensitive to snowfall and super-cooled liquid water. Click [[instruments:mwr_references|here]] for a list of relevant references. For background information see the [[http://cfa.aquila.infn.it/wiki.eg-climet.org/index.php?title=Microwave_radiometer|EG-CLIMET wiki]].
 ==== MRR =====