This is
where warm dust is very bright, and the swirling pattern you see is from all that dust.
Not exact matches
As the climate
warms, researchers expect more
dusts to make their way aloft, possibly having impacts on precipitation by changing
where rain or snow falls.
Using the Large Binocular Telescope Interferometer, or LBTI, in Arizona, the HOSTS Survey determines the brightness and density of
warm dust floating in nearby stars» habitable zones,
where liquid water could exist on the surface of a planet.
Through absorption of sunlight, the
dust particles
warm the layer of the atmosphere
where they reside.
This survey is full of fleeting delights, including a huge floor stencil made with turmeric, a work whose
warm orange
dust originally covered the marble floors of the British School in Rome
where it was staged in 1991.
Other factors would include: — albedo shifts (both from ice > water, and from increased biological activity, and from edge melt revealing more land, and from more old
dust coming to the surface...); — direct effect of CO2 on ice (the former weakens the latter); — increasing, and increasingly
warm, rain fall on ice; — «stuck» weather systems bringing more and more
warm tropical air ever further toward the poles; — melting of sea ice shelf increasing mobility of glaciers; — sea water getting under parts of the ice sheets
where the base is below sea level; — melt water lubricating the ice sheet base; — changes in ocean currents -LRB-?)