Tropical Storm Thane (06B) in the Bay of Bengal, and Tropical Storm Benilde (04S) in the South Indian Ocan

December 28th, 2011
MTSAT-1R 10.8 µm IR channel images

MTSAT-1R 10.8 µm IR channel images

 

MTSAT-1R 10.8 µm IR channel images from the CIMSS Tropical Cyclones site (above) showed Category 1 Tropical Storm Thane (06B) in the Bay of Bengal, moving toward the east coast of India on 28 December 2011.

Contours of 850-200 hPa satellite-derived deep layer wind shear overlaid on MTSAT-1R 6.75 µm water vapor channel images (below) indicated that Thane was in an environment of low wind shear, which favored some intensification prior to making landfall.

MTSAT-1R 6.75 µm water vapor channel images + Deep layer wind shear

MTSAT-1R 6.75 µm water vapor channel images + Deep layer wind shear

It is interesting to note that the MIMIC Total Precipitable Water product (below) showed the northern counterclockwise circulation of Tropical Storm Thane and the southern clockwise circulation of Tropical Storm Four (04S) — each drawing moisture from the Inter-Tropical Convergence Zone (ITCZ).

MIMIC Total Precipitable Water product

MIMIC Total Precipitable Water product

===== 30 December Update =====

Tropical Storm 04 S intensified in a similar low wind shear environment, becoming Tropical Cyclone Benilde in the South Indian Ocean. Benilde was forecast to intensify, with wind gusts up to 140 knots. Meteosat-7 visible/shortwave IR images with an overlay of ASCAT scatterometer surface winds (below) showed the structure of Benilde.

Meteosat-7 visble/shortwave IR imagery + ASCAT surface winds

Meteosat-7 visble/shortwave IR imagery + ASCAT surface winds

Development of an unusal tropical cyclone in the Mediterranean Sea

November 8th, 2011
EUMETSAT Meteosat-9 10.8 µm IR images

EUMETSAT Meteosat-9 10.8 µm IR images

A sequence of EUMETSAT Meteosat-9 10.8 µm IR images at 6-hour intervals (above) showed the development of an unusual tropical cyclone over the western Mediterranean Sea during the 06 November – 08 November 2011 time period.

The tropical cyclone was designated “01M” in a bulletin issued by NOAA/NESDIS Satellie Analysis Branch at 18:19 UTC on 07 November:

TXMM21 KNES 071819
TCSMED

A. 01M (NONAME)

B. 07/1800Z

C. 41.1N

D. 5.3E

E. THREE/MET-9

F. T2.5/2.5/D1.5/24HRS

G. IR/EIR/SWIR

H. REMARKS…DT=2.5 BASED ON .5 BANDING ON LOG10 SPIRAL. PT=2.5. MET=2.0. FT IS BASED ON DT. DEEP CONVECTION HAS PERSISTED LONG ENOUGH AROUND THE LOW LEVEL CENTER FOR A TROPICAL CLASSIFICATION.

I. ADDL POSITIONS

NIL

…SCHWARTZ

Wind speeds were estimated to have reached 45 knots according to various satellite analysis techniques.

Shown below is a comparison of EUMETSAT Meteosat-9 0.64 µm visible channel images at 12:00 UTC on 07 November and 08 November.

EUMETSAT Meteosat-9 0.64 µm visble channel images at 12:00 UTC on 07 and 08 November

EUMETSAT Meteosat-9 0.64 µm visble channel images at 12:00 UTC on 07 and 08 November

Eruption of the Nabro volcano in Eritrea

June 14th, 2011
FY-2E 0.73 µm visible channel images (click image to play animation)

FY-2E 0.73 µm visible channel images (click image to play animation)

The Nabro volcano erupted in the northeast Africa country of Eritrea on 12 June 2011. An oblique view using the Chinese FY-2E satellite (positioned over the Equator at 105º East longitude) 0.73 µm visible channel data (above; click image to play animation) showed the volcanic plume streaming northwestward on 13 June (the Nabro volcano is located near the bottom center of the images. Note that the plume became much brighter on the visible images later in the day, due to forward scattering.

A sequence of EUMETSAT Meteosat-9 7.35 µm “water vapor channel” images (below; click image to play animation) was useful for following the leading edge of the volcanic plume (the volcano summit is circled on the first few images of the animation). The plume moved northward over far northeastern Africa, and eventually curved anticyclonically and passed over the northern Arabian Peninsula on 14 June. It then appeared as if the leading edge of the volcanic plume might have eventually become entrained into a conveyor of isentropic ascent, where moisture began to increase (exhibiting a darker blue color on the water vapor images).

Meteosat-9 7.35 µm water vapor channel images (click image to play animation)

Meteosat-9 7.35 µm water vapor channel images (click image to play animation)