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Displaying all NUCAPS profiles from a single granule

As noted here, CIMSS scientist Tim Wagner has created a short python script to read NUCAPS files generated by Community Satellite Processing Package CSPP software and Direct Broadcast (DB) data at UW-Madison CIMSS. The script relies upon several python packages: netCDF4 (version 1.5.7), matplotlib (version 3.4.2), numpy (version 1.21.0) and... Read More

NOAA-20 NUCAPS Profiles over the USA Great Plains, 0845 UTC on 2 July 2021 (Click to enlarge)

As noted here, CIMSS scientist Tim Wagner has created a short python script to read NUCAPS files generated by Community Satellite Processing Package CSPP software and Direct Broadcast (DB) data at UW-Madison CIMSS. The script relies upon several python packages: netCDF4 (version 1.5.7), matplotlib (version 3.4.2), numpy (version 1.21.0) and sharppy. DB NUCAPS files are available from https://ftp.ssec.wisc.edu/pub/eosdb/j01/crisfsr/yyyy_mm_dd_jday_hhmm/edr/ ; Files have names like this:  NUCAPS-EDR_v2r0_j01_s202107020845119_e202107020845417_c202107020928000.nc (similar to the naming convention in NOAA CLASS); the filename above contains one data granule from 08:45:11.9 to 08:45:41.7 on 2 July 2021;  this orbital plot (from here) suggests that data is over the Great Plains of the United States.

The output from the python script is all the NUCAPS profiles from the granule.  There are 30 NUCAPS profiles for each scan line, and 4 scan lines per granule. The animation at top shows the soundings along with a mapping showing their location.

This retrieval of NUCAPS profiles occurred on a quiet weather day: the NUCAPS plot of sounding availability (here) showed mostly ‘green’ points (vs. yellow or red), signifying convergence in the infrared retrieval.  The image below compares the NUCAPS sounding in AWIPS (left) with the one processed via CSPP.  There is good agreement.

NOAA-20 NUCAPS Plot from AWIPS (left) and from CSPP (right) at 0845 UTC on 2 July 2021 for a point near the Nebraska/South Dakota/Wyoming border (Click to enlarge)[/caption

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Tropical Storm Elsa forms in the Atlantic

https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2021/07/Elsa_CSPP-GeoSphere.mp4Night Time Microphysics (at night) and True-Color imagery (during the day) over the eastern Atlantic, 0920 – 1220 UTC on 1 July 2021Tropical Storm Elsa has formed over the tropical eastern Atlantic Ocean.  True-color imagery from CSPP Geosphere (link) shows the storm with occasional bursts of deep convection.  Elsa has... Read More

Night Time Microphysics (at night) and True-Color imagery (during the day) over the eastern Atlantic, 0920 – 1220 UTC on 1 July 2021

Tropical Storm Elsa has formed over the tropical eastern Atlantic Ocean.  True-color imagery from CSPP Geosphere (link) shows the storm with occasional bursts of deep convection.  Elsa has formed at the southern edge of a large area of Saharan Air (shown below, link, from this site), and the storm’s future could be influenced by this dry air.

Saharan Air Layer analysis, 1200 UTC on 1 July 2021 (Click to enlarge)

The abundant dry air to the north of Elsa is also apparent in the low-level water vapor imagery, as shown below.

GOES-16 ABI infrared low-level water vapor (Band 10, 7.34 µm) at 1240 UTC on 1 July 2021. NHC prediction of the 1300 UTC position of Elsa along with 34-knot wind radii are shown (Click to enlarge)

The dry air associated with the SAL shows up nicely in gridded NUCAPS fields, too. The toggle below steps through the CIMSS True Color RGB and GOES-16 Band 10 imagery (7.34 µm) along with 850-700 mb relative humidity from gridded NUCAPS.

CIMSS True Color RGB, GOES-16 ABI Band 10 infrared water vapor (7.34 µm), 850-700 mb relative humidity, 1510 UTC on 1 July 2021 (Click to enlarge)

For more information on Elsa, see the SSEC Tropical Website. Official forecasts are on the website of the National Hurricane Center (link; direct link to Elsa’s webpages there)

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Pyrocumulonimbus clouds over British Columbia and California

GOES-17 (GOES-West) “Red” Visible (0.64 µm), Shortwave Infrared (3.9 µm) and “Clean” Infrared Window (10.35 µm) images (above) showed the explosive formation of large pyrocumulonimbus (pyroCb) clouds that were spawned by large wildfires in British Columbia, Canada on 30 June 2021. The 10.35 µm cloud-top infrared brightness temperatures rapidly cooled to the -50 to -60ºC range,... Read More

GOES-17 “Red” Visible (0.64 µm, top), Shortwave Infrared (3.9 µm, middle) and “Clean” Infrared Window (10.35 µm, bottom) [click to play animation | MP4]

GOES-17 “Red” Visible (0.64 µm, top), Shortwave Infrared (3.9 µm, middle) and “Clean” Infrared Window (10.35 µm, bottom) [click to play animation | MP4]

GOES-17 (GOES-West) “Red” Visible (0.64 µm), Shortwave Infrared (3.9 µm) and “Clean” Infrared Window (10.35 µm) images (above) showed the explosive formation of large pyrocumulonimbus (pyroCb) clouds that were spawned by large wildfires in British Columbia, Canada on 30 June 2021. The 10.35 µm cloud-top infrared brightness temperatures rapidly cooled to the -50 to -60ºC range, easily surpassing the -40ºC pyroCb threshold — and pyroCb 3.9 µm cloud-top infrared brightness temperatures were warmer (darker shades of gray) than those of surrounding meteorological cumulonimbus clouds (due to the presence of smaller ice crystals and smoke particles, which were better reflectors of incoming solar radiation).

GOES-17 Fire Temperature RGB images (below) include surface reports plotted in yellow — note that the temperature reached 115ºF (46.1ºC) at Kamloops (CYKA), just southeast of the largest fire. In addition, farther to the southwest, surface observations at Lytton (CWLY) ceased as of 01 UTC (6 PM local time), as another wildfire began to destroy 90% of that town.

GOES-17 Fire Temperature RGB images, with surface reports plotted in yellow [click to play animation | MP4]

GOES-17 Fire Temperature RGB images, with surface reports plotted in yellow [click to play animation | MP4]

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GOES-17 “Red” Visible (0.64 µm, top), Shortwave Infrared (3.9 µm, middle) and “Clean” Infrared Window (10.35 µm, bottom) [click to play animation | MP4]

GOES-17 “Red” Visible (0.64 µm, top), Shortwave Infrared (3.9 µm, middle) and “Clean” Infrared Window (10.35 µm, bottom) [click to play animation | MP4]

On a smaller spatial and temporal scale, GOES-17 Visible, Shortwave Infrared and Infrared Window images (above) revealed the brief formation of a pyroCb that was produced by the Lava Fire in far northern California. A portion of the cloud top reached the -40ºC threshold (darker shades of blue) to qualify as a pyroCb.

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Subtropical storm Raoni off the coast of South America

GOES-16 (GOES-East) “Red” Visible (0.64 µm) images (above) showed the circulation of Subtropical Storm Raoni (discussion issued by MARINHA) off the coast of Argentina/Uruguay on 28 June 2021.In the corresponding GOES-16 “Clean” Infrared Window (10.35 µm) images (below), the coldest cloud tops exhibited infrared brightness temperatures around -50ºC (shades of yellow).===== 29 June Update =====GOES-16 Visible... Read More

GOES-16 “Red” Visible (0.64 µm) images [click to play animation | MP4]

GOES-16 “Red” Visible (0.64 µm) images [click to play animation | MP4]

GOES-16 (GOES-East) “Red” Visible (0.64 µm) images (above) showed the circulation of Subtropical Storm Raoni (discussion issued by MARINHA) off the coast of Argentina/Uruguay on 28 June 2021.

In the corresponding GOES-16 “Clean” Infrared Window (10.35 µm) images (below), the coldest cloud tops exhibited infrared brightness temperatures around -50ºC (shades of yellow).

GOES-16 “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]

GOES-16 “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]

===== 29 June Update =====

GOES-16 “Red” Visible (0.64 µm) images [click to play animation | MP4]

GOES-16 “Red” Visible (0.64 µm) images [click to play animation | MP4]

GOES-16 Visible images (above) showed that Subtropical storm Raoni continued its northeastward motion, and was located off the coast of far southeastern Brazil on 29 June (12 UTC surface analysis | discussion).

GOES-16 Infrared images (below) indicated that Raoni was unable to maintain a persistent closed ring of cold clouds around its center.

GOES-16 “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]

GOES-16 “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]

A sequence of ASCAT surface scatterometer winds (source) from Metop-A and Metop-C (below) revealed swaths of wind speeds of 40 knots or greater within the northeastern and southwestern sectors of the system.

ASCAT winds from Metop-A and Metop-C [click to enlarge]

ASCAT winds from Metop-A and Metop-C [click to enlarge]

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