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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br /> Table 2. NOAA/Utah Radiometer Atmospheric Retrieval Coefficients <br />Year Ht./- CL1/CV1 CL2/C:V2 CL3/CV3 TMR20 TMR30 <br /> Type <br />1991 1784 -0.010740 -0.079233 0.49408 262.225 259.141 <br /> "all" <br /> n=50 0.016267 29.328 -12.954 <br />1991 2698 -0.0083351 0.0064490 0.43280 258.083 255.806 <br /> "all" <br /> n=50 0.019455 28.746 -12.770 <br />1991 2698 -0.0092847 0.0393EI1 0.412435 259.82 257.82 <br /> "Wet" <br /> n=33 0.018346 28.982 -12.891 <br />1991 2698 -0.0039208 -0.30324 0.52433 252.982 250.138 <br /> "dry" <br /> n=16 0.035886 27.294 -12.307 <br />1994 1784 -0.010087 -0.092282 0.48299 260.757 258.615 <br /> "all" <br /> n=30 0.025936 29.051 -12.933 <br />1994 2982 -0.0061925 -0.018855 0.41453 255.526 254.066 <br /> "all" <br /> n=30 0.026826 28.483 -12.832 <br />1991 & 1784 -0.010941 -0.05815 0.47571 261.676 259.148 <br />1994 "all" <br /> n=80 0.018804 29.290 -12.983 <br />1991 & 2982 -0.0072305 0.053n6 0.38962 256.218 254.329 <br />1994 "all" <br /> n=80 0.021449 28.768 -12.890 <br />Ht = Heinht (m, MSL) at which sounding processing was initiated <br />Type = Type of sounding: wet = >.3cm vapor; dry = <.3cm vapor; all = all sondes <br />n = Number of soundings in sample <br /> <br />Similar analyses were done for the liquid coefficients CL 1 J CL2 and CL3. These <br />results appear in Fig. 3. Here all coefficients show a very good linear trend with altitude <br />and indicate that linear expressions for TMR20, TMR30 and the liquid coefficients can be <br /> <br />8 <br />