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Validation Specialized ground based instruments are better suited for observing fog, but are extremely limited by their lack of spatial coverage. Conventional.

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Presentation on theme: "Validation Specialized ground based instruments are better suited for observing fog, but are extremely limited by their lack of spatial coverage. Conventional."— Presentation transcript:

1 Validation Specialized ground based instruments are better suited for observing fog, but are extremely limited by their lack of spatial coverage. Conventional surface observations are generally limited to populated areas (e.g. very few maritime observations) and are sometimes difficult to physically interpret. Despite the limitations of each data source, we will try to take advantage of the strength of each potential validation data set. Validation results are summarized on the next several slides.

2 Validation (fog/low stratus detection)
Accuracy statistics as a function of FLS probability threshold LIFR Probability (All Clds) IFR Probability (All Clds) MVFR Probability (All Clds) LIFR Probability (Liq. Clds) IFR Probability (Liq. Clds) MVFR Probability (Liq. Clds)

3 Validation (fog/low stratus detection)
Max. Algorithm Accuracy (threshold) LIFR All Pixels Liquid Pixels Only Daytime LIFR 93.1% (32%) 95.9% (74%) Nighttime LIFR 89.7% (46%) 91.0% (48%) Terminator LIFR 88.3% (32%) 89.7% (47%) IFR All Pixels Liquid Pixels Only Daytime IFR 90.6% (55%) 93.8% (60%) Nighttime IFR 87.5% (48%) 89.9% (62%) Terminator IFR 85.8% (48%) 88.2% (60%) MVFR All Pixels Liquid Pixels Only Daytime MVFR 85.1% (69%) 88.1% (74%) Nighttime MVFR 85.0% (55%) 88.3% (61%) Terminator MVFR 82.6% (61%) 85.2% (61%) # of pts All Pixels Liquid Pixels Only Daytime 492,977 298,480 Nighttime 564,029 278,042 Terminator 92,654 49,083 The validation data set was comprised of 12, 24-hr periods (1 day from each month) of GOES-13 data collocated with surface observations The accuracy of the Enterprise GS LIFR, IFR and MVFR algorithms exceed the 70% F&PS accuracy specification during both day and night.

4 Validation (fog/low stratus detection)
CSI statistics as a function of FLS probability threshold LIFR Probability (All Clds) IFR Probability (All Clds) MVFR Probability (All Clds) LIFR Probability (Liq. Clds) IFR Probability (Liq. Clds) MVFR Probability (Liq. Clds)

5 Validation (fog/low stratus detection)
Algorithm Accuracy at Max CSI (threshold) LIFR All Pixels Liquid Pixels Only Daytime LIFR 91.4% (9%) 94.0% (9%) Nighttime LIFR 85.5% (12%) 87.8% (13%) Terminator LIFR 84.6% (9%) 86.9% (10%) IFR All Pixels Liquid Pixels Only Daytime IFR 89.0% (33%) 92.8% (36%) Nighttime IFR 85.4% (26%) 88.2% (31%) Terminator IFR 83.6% (28%) 86.8% (30%) MVFR All Pixels Liquid Pixels Only Daytime MVFR 84.2% (57%) 86.9% (58%) Nighttime MVFR 84.0% (43%) 87.1% (47%) Terminator MVFR 81.6% (47%) 83.7% (47%) # of pts All Pixels Liquid Pixels Only Daytime 492,977 298,480 Nighttime 564,029 278,042 Terminator 92,654 49,083 The validation data set was comprised of 12, 24-hr periods (1 day from each month) of GOES-13 data collocated with surface observations Even at the probability threshold that yields the highest CSI (skill) the accuracy of the Enterprise GS LIFR, IFR and MVFR algorithms exceed the 70% F&PS accuracy specification during both day and night.

6 Validation (fog/low stratus detection)
Nighttime Reliability tables LIFR IFR MVFR

7 Validation (fog/low stratus detection)
Daytime Reliability tables LIFR IFR MVFR

8 Validation (fog/low stratus detection)
Terminator Reliability tables LIFR IFR MVFR

9 Validation The acoustic SODAR (Sonic Detection And Ranging) is an upwardly pointing parabolic antenna that emits an audible signal whose return signal is proportional to the vertical gradient of air density. As such, the SODAR is capable of detecting the base of the inversion, which defines the top of the stratus deck. A combination of ceilometer and SODAR measurements are used to infer the geometric boundaries of low clouds in the San Francisco Bay Area. This network of instruments is operated by the FAA and NWS.

10 Validation The combination of SODAR and ceilometer data can be used to validate the fog depth product. fog depth

11 Validation (fog depth)
Initial performance estimates indicate that the 500 m accuracy will be readily achieved (bias < 32 m). The strong correlations indicate that the spatial and temporal patterns are informative. Daytime Nighttime

12 Validation: Summary The validation of the fog/low stratus products show that: The fog depth algorithm easily meets the 500 m accuracy requirement. The LIFR, IFR and MVFR probability products easily meet the 70% accuracy requirement


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