AVHRR false color imagery (above; viewed using Google Earth) and GOES-11 visible channel imagery (below) revealed a family of cyclonic vorticiesÂ propagating westward across the eastern North Pacific Ocean on 29 March 2008. The radially-banded cloud features that form such cloud â€œswirlsâ€ are known as actinae or actinoform clouds, and they are seen occasionally in the marine stratocumulus cloud field over the Pacific Ocean (for example, other similar cases were observed in March 2007 and June 1997). This type of cloud pattern was first observed on TIROS V imagery way back in August 1962 and October 1962.
GOES-11 visible channel (daytime) and 3.9 Âµm shortwave IR (nighttime) imagery revealed an interesting cyclonic vortex which was propagating westward across the eastern North Pacific Ocean on 13-14 March 2007 (Java animation | QuickTime animation). The radial banded cloud features that form such a cloud “swirl” are known as actinae or actinoform clouds, and they are seen occasionally in the marine stratocumulus cloud field over the Pacific Ocean (one such case was June 1997). This type of cloud pattern was first observed back in 1962 on TIROS V imagery near Hawaii.
The GOES-14 (GOES-O) satellite was launched on 27 June 2009, and is undergoing its Post Launch Test. The first calibrated full disk visible image (above) was received by the SSEC Data Center beginning at 17:30 UTC on 27 July 2009.
A close-up view centered over central California (below) showed marine fog and stratus hugging the Pacific coast, with cumulus clouds developing inland over the higher terrain of the Sierra Nevada.
Farther to the west, a pattern of ship tracks was evident in the marine layer stratocumulus clouds over the North Pacific Ocean (below).
A nice series of von Karman vorticies was seen streaming southward from Guadalupe Island off the west coast of Baja California (below).
A view centered over southern Florida (below) showed the development of numerous thunderstorms over that region.
A view centered over Lake Erie (below) showed widespread cumulus cloud development surrounding the lake (with some bands of billow clouds evident in the eastern portion of the scene). There was also a hint of a sediment plume south of Long Point, which extends into the northeastern portion of the lake from Ontario — this sediment plume could also be seen on MODIS true color imagery.
Looking to the south of the Equator, a view centered over central Chile in South America (below) showed a small cyclonic (clockwise in the Southern Hemisphere) vortex in the marine layer clouds off the coast, with snow cover inland over the higher terrain of the Andes.
Over the South Pacific Ocean, some interesting cloud structure suggesting the formation of actinae was apparent (below).
An image centered over the Amazon River in central Brazil (below) showed how the wide waterway was suppressing the formation of cumulus clouds (since the water surfaces were not heating up as quickly as the adjacent land surfaces). The Amazon River was still abnormally wide after record rainfall across parts of Brazil during May-June 2009 — in fact, at the mouth of the Amazon River a large sediment plume was seen fanning outward into the Atlantic Ocean on MODIS true color imagery.