GOES-14 SRSOR: Mesovortices in the eye of Hurricane Marie

August 25th, 2014
GOES-14 0.63 µm visible channel images (click to play YouTube video)

GOES-14 0.63 µm visible channel images (click to play YouTube video)

The GOES-14 satellite was in Super Rapid Scan Operations for GOES-R (SRSOR) mode, providing 1-minute interval images of Category 4 intensity Hurricane Marie over the East Pacific Ocean on 25 August 2014. Even though the eye was cloudy, the 1-minute imagery revealed a number of mesovortices circulating within the eye of Hurricane Marie (above; click image to play YouTube video). Note: the YouTube video is best viewed in Full Screen mode, and clicking on the “Gear” icon to select “1080p HD”.

On the previous day, the eye was less cloudy and mesovortices were more easily seen on GOES-15 0.63 µm visible channel images (below; click to play Animated GIF); however, the GOES-15 images were only available at the routine 15-minute interval, which made tracking the evolution and motion of the mesovortices more difficult. On this day (24 August) Hurricane Marie had rapidly intensified to a Category 5 storm (plot of CIMSS ADT).

GOES-15 0.63 µm visible channel images (click to play Animated GIF)

GOES-15 0.63 µm visible channel images (click to play Animated GIF)

The effect of wind shear on Tropical Storm Karina

August 24th, 2014
GOES-15 0.63 µm visible channel  images (click to play Animated GIF)

GOES-15 0.63 µm visible channel images (click to play Animated GIF)

GOES-15 0.63 µm visible channel images (Animated GIF | MP4 movie | YouTube video | QuickTime movie) showed the decoupling of the upper-level and lower-level circulations of Tropical Storm Karina in the East Pacific Ocean on 24 August 2014. This decoupling was caused by strong wind shear along the western periphery of Category 5 Hurricane Marie, which was located to the east-southeast of Karina (large-scale view). Kudos to Dennis Chesters (NASA/Goddard) for bringing this interesting case to our attention (and providing the QuickTime movie linked to above).

The corresponding GOES-15 10.7 µm IR channel images (Animated GIF | MP4 movie | YouTube video) showed the cold clouds (red to black to white to purple color enhancement) associated with the upper-level circulation moving northward and quickly dissipating; the signature of the warmer clouds (darker cyan color enhancement) associated with the lower-level circulation can also be seen emerging from beneath the cold cloud shield and moving eastward.

GOES-15 10.7 µm IR channel images (click to play Animated GIF)

GOES-15 10.7 µm IR channel images (click to play Animated GIF)

A closer view provided by a Suomi NPP VIIRS true-color Red/Green/Blue (RGB) image from the SSEC RealEarth web map server (below) showed the separation of the upper-level and lower-level circulations around 21:53 UTC.

Suomi NPP VIIRS true-color RGB image

Suomi NPP VIIRS true-color RGB image

A sequence of 4 images (15, 18, 21, and 00 UTC) from the CIMSS Tropical Cyclones site (below) shows GOES-15 6.5 µm water vapor channel images with overlays of deep-layer wind shear (derived from satellite winds). To the east of Karina (which was located in the center of the images), the large anticylcone aloft associated with Category 5 Hurricane Marie can be seen, with increasing vales of southeasterly wind shear moving over Karina.

GOES-15 6.5 µm water vapor images with overlays of deep layer wind shear

15 UTC GOES-15 6.5 µm water vapor images with overlays of deep layer wind shear

The 3 image comparisons below show the separation of the centers of upper-level divergence (yellow) and lower-level convergence (cyan) as the decoupling process was occurring at 18 UTC, 21 UTC, and 00 UTC.

18 UTC GOES-15 6.5 µm water vapor image with upper-level divergence (yellow) and GOES-15 10.7 µm IR image with lower-level convergence (cyan)

18 UTC: GOES-15 6.5 µm water vapor image with upper-level divergence (yellow) and GOES-15 10.7 µm IR image with lower-level convergence (cyan)

21 UTC: GOES-15 6.5 µm water vapor image with upper-level divergence (yellow) and GOES-15 10.7 µm IR image with lower-level convergence (cyan)

21 UTC: GOES-15 6.5 µm water vapor image with upper-level divergence (yellow) and GOES-15 10.7 µm IR image with lower-level convergence (cyan)

00 UTC: GOES-15 6.5 µm water vapor image with upper-level divergence (yellow) and GOES-15 10.7 µm IR image with lower-level convergence (cyan)

00 UTC: GOES-15 6.5 µm water vapor image with upper-level divergence (yellow) and GOES-15 10.7 µm IR image with lower-level convergence (cyan)

===== 25 August Update =====

GOES-15 0.63 µm visible channel images, with Metop ASCAT surface scatterometer winds

GOES-15 0.63 µm visible channel images, with Metop ASCAT surface scatterometer winds

Even though the southeastward-moving low-level circulation of Karina had been downgraded to a Tropical Depression with 30 knot winds, there was still an impressive burst of convection just west of the center as it began to move back over warmer water on 25 August. Metop ASCAT surface scatterometer winds (above) showed a small pocket of winds in the 30.0-39.9 knot range (green wind barbs) at 18:29 UTC.

There were also some Tropical Overshooting Top (TOT) targets detected within the convective burst (below); TOT symbols: Red = 0-1 hour previous, Green = 1-2 hours previous, Blue = 2-3 hours previous.

GOES-15 Infrared - Water Vapor difference product, and Tropical Overshooting Tops product (TOT symbols: Red = 0-1 hour previous, Green = 1-2 hours previous, Blue = 2-3 hours previous)

GOES-15 Infrared – Water Vapor difference product, and Tropical Overshooting Tops product (TOT symbols: Red = 0-1 hour previous, Green = 1-2 hours previous, Blue = 2-3 hours previous)

Mesovortices within the eye of Hurricane Lowell

August 21st, 2014
GOES-15 0.63 µm visible channel images (click to play animation)

GOES-15 0.63 µm visible channel images (click to play animation)

GOES-15 0.63 µm visible channel images (above; click image to play animation; also available as an MP4 movie file) revealed the presence of mesovortices within the eye of Category 1 Hurricane Lowell in the East Pacific Ocean on 21 August 2014.

The mesovortices were also evident at 21:07 UTC in a Suomi NPP VIIRS true-color image from the SSEC RealEarth web map server (below).

Suomi NPP VIIRS true-color image

Suomi NPP VIIRS true-color image

In addition to having a rather large eye, Hurricane Lowell also had a large radius of strong winds, as seen on a comparison of a GOES-15 0.63 µm visible image and Metop ASCAT surface scatterometer winds from the CIMSS Tropical Cyclones site (below).

GOES-15 0.63 µm visible channel image with Metop ASCAT surface scatterometer winds

GOES-15 0.63 µm visible channel image with Metop ASCAT surface scatterometer winds

GOES-14 SRSOR: Tropical Storm Lowell in the East Pacific Ocean

August 19th, 2014
GOES-14 0.63 µm visible channel images (click to play Animated GIF)

GOES-14 0.63 µm visible channel images (click to play Animated GIF)

The GOES-14 satellite was in Super Rapid Scan Operations for GOES-R (SRSOR) mode, providing coverage of Tropical Storm Lowell in the East Pacific Ocean on 19 August 2014; an animation of 0.63 µm visible channel images (Animated GIF | MP4 movie file | YouTube) showed a gradual increase in the organization of a convective banding structure during the day. At 12 UTC Tropical Storm Lowell was located several hundred miles southwest of Baja California, with a center at 15.5º North latitude, 119.5º West longitude.

GOES-15 10.7 µm IR channel images with an overlay of Metop ASCAT surface scatterometer winds from the CIMSS Tropical Cyclones site (below) showed the the strongest winds (40.0-49.9 knots, yellow barbs) were in the southeastern quadrant of Lowell at 17:11 UTC.

GOES-15 10.7 µm IR images with Metop ASCAT surface scatterometer winds

GOES-15 10.7 µm IR images with Metop ASCAT surface scatterometer winds

A comparison of the 16 UTC GOES-15 10.7 µm IR channel image with the corresponding DMSP SSMIS 85 GHz microwave image (below) indicated that the highest rainfall rates were associated with the convective banding  (and coldest cloud tops) within the southern semicircle of the storm.

GOES-15 10.7 µm IR image and DMSP SSMIS 85 GHz microwave image

GOES-15 10.7 µm IR image and DMSP SSMIS 85 GHz microwave image