This page provides information related to the development and testing of the Thin-cloud Rotating Shadowband Radiometer (TCRSR). This is a log for the development of the instrument. A good description of the instrument and data processing can be found in the SGP DATA REPORT. Certain details in the processing software can be found in BANDANGLES PROCESSING REPORT
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The logic design, shown here, should satisfy all fail-safe requirements with a minimum of complexity. |
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| Demonstration 1: A demonstration of the first phase of development of the TCRSR was conducted successfully at BNL on 25 July 2007. Attending were R. M. Reynolds, W. Wiscomb, A. Vogelmann, S. Smith (mechanical engr.), and R. Edwards (electronic engr.). |
The sky was clear and deep blue. We installed the TCRSR on the BNL roof test platform and operated it from 11:57:34 to 14:24:06 (EDT). There were some breaks in the data when the TT8 stopped for no apparent reason.
In all data presentation the 2 degree band is designated by 1 and the 5-degree band is designated by 2. The MFR head channels are labeled 0-7 for approximate input filters centered on [open,415,500,615,680,870,940]. The zeroth channel is the open silicone detector. Note these data are uncorrected for zenith angle, atmospheric mass, or sensor azimuth-elevation correction.
Another near-perfect sunny day.
Operation time: 2007-09-24 (267) 15:33:35 to 2007-09-24 (267) 18:41:43.
In all data presentation the 2 degree band is designated by 1 and the 5-degree band is designated by 2. The MFR head channels are labeled 0-7 for approximate input filters centered on [open,415,500,615,680,870,940]. The zeroth channel is the open silicone detector. Note these data are uncorrected for zenith angle, atmospheric mass, or sensor azimuth-elevation correction.
| SAME AS ABOVE |
| SAME AS ABOVE |
| SAME AS ABOVE |
On the morning of 6 October 2007, the TC-RSR was deployed at BNL to further test its operational stability while observing the burn off of fog. It began mid morning (before which the optical path was too great for an aureole to be exhibited in the scans) and progressed into early afternoon. Once the burn off reached a sufficiently small optical path, the Sun's aureole appeared. However, interestingly, its magnitude fluctuates during this later period, indicating that the fog has notable inhomogeneities as denser portions waft in and out of the field of view during the burn off.