Ship Tracks South of Alaska
Natural Color
acquired March 4, 2009 download large Natural Color image (3 MB, JPEG, 4892x4224)
acquired March 4, 2009 download Natural Color GeoTIFF file (48 MB, TIFF, 4892x4224)
Ship Tracks South of Alaska
Cloud Droplet Radius
Color bar for Ship Tracks South of Alaska
acquired March 4, 2009 download large Cloud Droplet Radius image (679 KB, JPEG, 1223x1056)
acquired March 4, 2009 download Cloud Effective Radius GeoTIFF file (2 MB, TIFF, 1223x1056)
acquired March 4, 2009 download Google Earth file (KML)

On March 4, 2009, the skies over the northeast Pacific Ocean were streaked with clouds that form around the particles in ship exhaust. This pair of images shows how these ship tracks are different from the natural marine clouds in the same area. The top image is a natural-color (photo-like) view of the ship tracks. The image below reveals more information than a picture: it shows the size of the cloud droplets. Both images are based on observations made by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite.

In the natural-color view of the clouds, the ship tracks are noticeably brighter than the natural marine clouds. What makes one cloud brighter than another? The bottom image reveals one of the important influences on brightness: the size (radius) of the droplets in the cloud. The ship tracks are brighter than the regular clouds because the cloud particles in them are smaller (yellow and peach), but more numerous, than the particles in the natural clouds (lavender to dark purple).

Cloud droplets form when water vapor condenses (or nucleates) onto a small particle, like an aerosol particle produced from fossil fuel combustion or a salt crystal from the ocean surface. The more numerous the nucleation “seeds,” the more numerous the cloud droplets, and the smaller the resulting droplet size because the available condensed water is partitioned among a great number of droplets. The particles produced in ship exhaust are more numerous than the natural aerosols over the ocean. So the clouds that form in the plumes of ships have more, smaller droplets than the background marine clouds.

The two cloud regions (in-track and out-of-track) may actually contain the same volume of water. But a volume of cloud water condensed onto many small droplets has a larger reflective cross sectional area than an equal amount of water condensed into fewer, but larger droplets. (Said another way, as the radius of a sphere—a cloud droplet—gets smaller, surface area decreases more slowly than volume.) Because more light is reflected back to the satellite, the cloud with smaller droplets looks brighter.

Why are scientists concerned with cloud brightness? A cloud’s brightness impacts how much sunlight gets bounced back to space and how much reaches the surface of the Earth, which influences global climate. The size of the droplets also influences the amount of rain the clouds produce; smaller droplets are less likely to collide and form drops that are big enough to fall as rain.

NASA images by Robert Simmon and Jesse Allen, based on an image by Jeff Schmaltz, MODIS Rapid Response Team. Caption by Rebecca Lindsey.

Instrument(s): 
Terra - MODIS

Ship Tracks South of Alaska

March 12, 2009
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