Archive for the ‘Marine weather’ Category

Unusual August ice concentration in Hudson Bay and James Bay, Canada

Monday, August 10th, 2009
MODIS true color and false color images

MODIS true color and false color images

A comparison of MODIS “true color” and “false color” Red/Green/Blue (RGB) images (above) showed that significant amounts of ice remained in parts of southern Hudson Bay and northern James Bay in Canada on 10 August 2009. On the true color RGB image (using MODIS bands 01/04/03), the ice did not appear as as bright as the surrounding clouds, and had a slightly “light blue” appearance. On theĀ  false color RGB image (using MODIS bands 02/07/07), the ice (along with clouds that were composed of ice crystals) exhibited a darker red appearance, in contrast to the cyan to white colored supercooled water droplet clouds.

Also note the hazy appearance over parts of Ontario, just to the west of James Bay: this was due to smoke aloft from recent fire activity in Alaska and the Yukon Territory.

A map of the departure from normal ice concentration (below, courtesy of the Canadian Ice Service) indicated that there were large areas where the iceĀ  was in the 7/10ths to 10/10ths range above the normal concentration for the date (darker blue colors). The persistence of a deep area of low pressure just south of Hudson Bay (July 2009 mean 850 hPa geopotential height) kept that region (along with much of the eastern US) unusually cold during the summer, which undoubtedly slowed the rate of ice melt in Hudson Bay and James Bay.

Ice Concentration departure from normal

Ice Concentration (departure from normal)

Lake Superior lake breeze

Monday, June 22nd, 2009
GOES-12 visible images

GOES-12 visible images

GOES-12 visible images (above) showed that a well-defined lake breeze developed along the western portion of Lake Superior during the afternoon hours on 22 June 2009. The MODIS Sea Surface Temperature (SST) product from 2 days earlier (below) indicated that SST values in the much of the middle of the lake were still in the low 40s F (blue color enhancement) — and Buoy 45006 was actually reporting a SST value of 39 F on 22 June. In northern Wisconsin, note the large surface air temperature gradient that existed between Port Wing (station identifier PNGW3) which remained in the upper 40s F and Ashland (station identifier KASX) which rose into the low 80s F!

MODIS Sea Surface Temperature product

MODIS Sea Surface Temperature product

Farther to the south, GOES-12 visible imagery also showed that a Lake Michigan lake breeze was moving inland across southeastern Wisconsin and northeastern Illinois (below).

GOES-12 visible image

GOES-12 visible image