The discussion section of the very recent, on-line-available Terrestrial glint seen from deep space: oriented ice crystals detected from the Lagrangian point Alexander Marshak, Tamás Várnai and Alexander Kostinski, doi: 10.1002/2017GL073248 contains the following text:

Based on in-situ measurements of cirrus clouds, [Korolev et al., 2000; McFarquhar et al., 2002], tiny hexagonal platelets of ice, floating in air in nearly perfect horizontal alignment, are likely responsible for the glints observed by EPIC over land. Because the EPIC instrument has a field of view of 0.62 degrees (see, and a 2048x2048 pixels CCD, the specular signal within an angle of only $~3x10^{-4}$ degree (Fig. 2) must either contain smooth large oriented ice plates or smaller oriented platelets sending back diffracted light. Size distribution of such crystals depends greatly on cloud temperature and humidity but the range is from tens of microns to mm. Taking the wavelength of 0.5 micron and ice platelet size of 50 microns, yields the ratio or angular half-width of the diffraction lobe around the specular direction $10^{-2}$ or on the order of a degree [Crawford, 1968, p.486]. This is broader than the angular width of a pixel but narrower than change in the zenith direction over the area covered by a pixel (0.1°).

In other words, if the ice plates are parallel to the local surface of the Earth, the curvature of the Earth itself results in the observed specular reflection being localized to an area tens of kilometers wide at a distance of 1.5 billion kilometers, despite the assumed size of 50 microns and it's large diffraction half-angle of order tenths of a degree.

To roughly summarize the explanation, there are flat plates of ice crystals above 5 km in thin atmospheric clouds that tend to orient themselves very horizontally - parallel to the local surface of the Earth - most of the individual plates would each need to be horizontal within a small fraction of one degree, not just on average. Every azimuthal degree along the Earth's surface is about 111 kilometers, so if the glints are just for example 1 pixel or about 10 kilometers wide, it means there is something selecting the angle within about 0.1 degrees. That could be the diffraction limit of something - perhaps a little bigger than the 50 microns mentioned but could certainly be smaller than the limit of order a millimeter as mentioned.

However, The source of the illumination is the Sun, and as seen from Earth the width is about a half of a degree. You have to divide that by a factor of 2 because we're talking about "the mirror tilting", not the incident angle, but that would still correspond to a width of 111 km times 0.53 degree times one-half, or about 29.5 kilometers minimum size, no matter how large and perfectly horizontal the plates, wouldn't it?

Due to the finite apparent size of the sun as seen by DSCOVR reflected in even a perfect mirror in the Earth's atmosphere following the curvature of the Earth, wouldn't the apparent size/shape be a uniform spot with a diameter of ~30 kilometers, and always almost four ~ 8 km pixels wide if not larger in the un-binned 2048x2048 pixel DSCOVR images?

You can't forget that there still are the following widening mechanisms that are also contributing at some level:

  • Diffraction from the finite sizes of the ice plates. Slightly smaller plates would enlarge the spot, while substantially smaller plates would produce a much larger area but with correspondingly lower brightness per unit area and therefore be undetected, so it's only the (roughly speaking) say 20-50 micron sized hexagonal plates that must be absent to avoid widening of the apparent spot.
  • Imperfect "horizontality" or more precisely; plate-to-plate fluctuations from co-planarity.
  • DSCOVR optics? I don't know if the regularly obtained resolution in practice is always below one pixel under these conditions, perhaps it is.

I don't think the cause is a clever PrankSat nor some clever people with a lot of extra frequent flyer miles and aluminum foil, and the upper atmospheric ice plate thesis has a lot of merit, but I still can't reconcile the 0°.53 equatorial width of the sun's rays at the distance of a reflection from Earth from DSCOVR (e.g. 1 AU + 1.5 million km) with the near-single-pixel observations in the blue channel. Am I just missing something here?

Note: It is only the blue channel (about 443nm) that is routinely transmitted to Earth in full resolution. Pixel size estimates (note the arrow in the annotated cropped image below) should only be applied to images in the full resolution blue channel.

Out of total 4106 images collected, 336 contain land-glint for the blue channel, which was chosen because it has the highest spatial resolution (to reduce the amount of data transmitted from DSCOVR, for all other channels four pixels are averaged onboard the spacecraft).

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For anyone who would like to approach the math in a systematic way, the question would be about how large the virtual image of the sun would appear to DSCOVR to be if reflected in a convex spherical mirror centered at the center of the earth with a radius equal to 6378 + 5 kilometers. Would it look like it is about 30 kilometers in diameter if projected to the point of reflection, if you treat it as if it were on the surface of the mirror itself?

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above: From slide #12 here (after you wait for the fade-in). For this question, imagine the camera shown in this image is closer to the mirror than the candle - the candle, representing the sun, would be behind the camera, representing DSCOVR's camera EPIC.

  • This previous, related question is about the linked previous explanation (Cassegrain optics and coherent backscattering). This question here is about the recently described "NASA" explanation of extremely horizontal ice plates within thin clouds above 5 km. – uhoh May 21 '17 at 8:19
  • I'd add a bounty but people keep ignoring them! – uhoh May 21 '17 at 8:41
  • Sometimes people reflexively down vote anything that questions any aspect of any technical result from NASA assuming that they must be a hoax-believer. I'm not. I would simply like to understand how the explanation matches physics. if "too difficult or detailed" is off-topic, please let me know! But i think the optics in my question is correct, and the spots, as explained, can't be so small. I think these flashes are fascinating, and I'd really like to understand their cause! – uhoh May 21 '17 at 10:14
up vote 2 down vote accepted

An additional factor resulting in small (and even single pixel) glints is that the horizontally oriented ice crystals may cover only a small region. For example an ice cloud may be small, or ice crystals in the rest of a large cloud may be oriented randomly (as opposed to horizontally) as they tumble through the air.

  • 1
    Welcome to stack exchange - it's always great when the author of the paper being discussed shows up to comment on their work! I have a hunch you guys are continuing to pursue studies of this intriguing phenomenon, if there are any developments in the future I hope you'll have time to stop by and leave an update, or a link to any newer papers or talks. DSCOVR just keeps generating an ever-increasing body of data with its constant stare at Earth's sunlit disk. – uhoh Jun 16 '17 at 22:09

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