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Measurement uncertainties of scanning microwave radiometers and their influence on temperature profiling

Pub­lished in Atmos. Meas. Tech., 17, 219–233, 2024:

In order to improve obser­va­tions of the atmos­pher­ic bound­ary lay­er (ABL), the Euro­pean Mete­o­ro­log­i­cal Net­work, EUMETNET, and the Aerosol, Clouds, and Trace Gas­es Research Infra­struc­ture, ACTRIS, are cur­rent­ly work­ing on build­ing net­works of microwave radiome­ters (MWRs). Ele­va­tion-scan­ning MWRs are well suit­ed to obtain tem­per­a­ture pro­files of the atmos­phere, espe­cial­ly with­in the ABL. Under­stand­ing and assess­ing mea­sure­ment uncer­tain­ties of state-of-the-art scan­ning MWRs is there­fore cru­cial for accu­rate tem­per­a­ture pro­fil­ing. In this paper, we dis­cuss mea­sure­ment uncer­tain­ties due to the instru­ment set­up and orig­i­nat­ing from exter­nal sources, name­ly (1) hor­i­zon­tal inho­mo­geneities of the atmos­phere, (2) point­ing errors or a tilt of the instru­ment, (3) phys­i­cal obsta­cles in the line of sight of the instru­ment, and (4) radio fre­quen­cy inter­fer­ence (RFI). Hor­i­zon­tal inho­mo­geneities from obser­va­tions at the Jülich Obser­va­to­ry for Cloud Evo­lu­tion (JOYCE) are shown to have a small impact on retrieved tem­per­a­ture pro­files ( in the 25th and 75th per­centiles below 3000 m). Typ­i­cal instru­ment tilts, that could be caused by uncer­tain­ties dur­ing the instru­ment set­up, also have a very small impact on tem­per­a­ture pro­files and are small­er than 0.1 K below 3000 m for up to 1 of tilt. Phys­i­cal obsta­cles at ambi­ent tem­per­a­tures and in the line of sight and fill­ing the com­plete beam of the MWR at the low­est ele­va­tion angle of 5.4 have to be at least 600 m away from the instru­ment in order to have an impact of less than 0.1 K on obtained tem­per­a­ture pro­files. If the obsta­cle is 5 K warmer than its sur­round­ings then the obsta­cle should be at least 2700 m away. Final­ly, we present an approach on how to detect RFI with an MWR with azimuth and ele­va­tion-scan­ning capa­bil­i­ties. In this study, we detect RFIs in a water vapor chan­nel that does not influ­ence tem­per­a­ture retrievals but would be rel­e­vant if the MWR were used to detect hor­i­zon­tal humid­i­ty inho­mo­geneities.

Authors: Tobias Böck, Bern­hard Pospichal, and Ulrich Löh­n­ert

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