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<br />~ <br />..- <br /> <br /> ~ <br /> ..- I~ <br /> en <br />- Q <br />E <br />(J <br />- <br />~ <br />0 <br />~ CD <br />~ Q <br />~ <br />CI) <br />.... <br />ca <br />3: <br /> M <br /> Q <br /> <br /> <br />Q <br />Q <br /> <br /> <br />14 <br /> <br />16 <br /> <br />18 <br /> <br />20 <br /> <br />22 <br /> <br />24 <br /> <br />02 <br /> <br />en <br />- Q <br />E <br />E <br />- <br />a.. <br />.s <br />ca <br />3= <br />:E <br />= <br />tr' <br />:::i <br /> <br />CD <br />Q <br /> <br />M <br />Q <br /> <br />08 <br /> <br /> <br />14 <br /> <br />16 <br /> <br />18 20 22 <br />Time (UTe) <br /> <br />24 <br /> <br />02 <br /> <br />04 <br /> <br />06 <br /> <br />....1!1 <br />,",0 <br /> <br />Q <br />Q <br /> <br />10 <br /> <br />Figure 2.8. - Example of vertically integrated liquid water (bottom) and water vapor (top) observed by the radiometer <br />on February 18, 1992. over Johnsville. The spikes in the liquid data show enhanced liquid over Grizzly Ridge as the <br />antenna scanned over this location. Vaiues have been normalized to the vertical. PST (Pacific standard time) is UTe <br />minus 8 h. <br /> <br />16 <br />