Showing posts with label superparhelia. Show all posts
Showing posts with label superparhelia. Show all posts

Thursday, 21 January 2021

Streetlight halos in Lahti, 17 January 2021

After having spotted reasonably thick diamond dust from a distance while taking the sheepdog out, I spent good few hours outdoors observing and photographing divergent light halos in the surroundings of Pikku Vesijärvi park in Lahti, Southern Finland. As is generally the case in urban areas in this country, there were many lamp posts to choose from, but few of them provided any sort of darkish background for serious observing. Much of my time went into finding good spots and chasing the best swarm of ice crystals while also trying to avoid crowds of people. I found quite good conditions in the harbour area: very quiet this time of year but the lights along a boulevard are being kept switched on. For the best results I chose a lamp at the far end of the boulevard with nothing but a lake in the background.

Based on my visual observations, much of the display was dominated by singly-oriented column crystals with additional contributions from plate crystals at times. Temperature at the nearby Sopenkorpi weather station varied in the range of -7°C to -9°C.

The photo above is an unsharp-masked stack that consists of 10 individual 30 second exposures and covers some 10 minutes at around 9:15 pm local time. My interpretation of the photo is as follows:

  • The Y-shape above the lamp is the divergent light version of the upper tangent arc.
  • The horizontal arcs to the left and right of the lamp are the divergent parhelia.
  • The vertical line pointing to the top of the frame is the superlamp.
  • The curved lines pointing approximately to 11 and 1 positions from the lamp are the superparhelia.
  • Of the pair of arcs at 10 and 2 positions from the lamp, the one that goes above the other is the helic arc.

Some uncertainty remains on the identification of the arc immediately below the helic arc. Nicolas Lefaudeux (personal communication) has kindly offered two possible explanations that are both supported by his atlas of divergent light halo simulations: Firstly, corresponding to a hypothesis of singly-oriented column crystals (and the interpretation that the Y-shaped arc indeed is the upper tangent arc), this arc would be the divergent light version of Wegener arc. For the other possibility, we replace the idea of singly-oriented column crystals by Parry orientation, which means that the Y-shape would come from the upper sunvex Parry arc. The oblique arc below the helic would then be divergent light Hastings arc, potentially with a contribution from Tape arc, as the two overlap in the simulation.

The relatively strong presence of helic arc provides some support to the Hastings/Tape option. On the other hand, from what I could see visually for the most parts of the display, I would feel uneasy to exclude the presence of singly-oriented crystals altogether. The smart-phone photo below illustrates my point: the sparkles above the floodlight make no resemblance to Parry, but instead look much like upper tangent arc. Therefore I feel that at least part of the intensity is likely to come from the Wegener option.


Thursday, 9 February 2017

Observing diamond dust halos at the Bílá ski centre

Superparhelia and sharp light pillars
Taken by Daniel Neumann

At the night between 18th and 19th January 2017 me and my friend Daniel decided to try our luck and head towards the Bílá ski centre (approx. 50 km away). Before we headed out, we checked the webcams located at the centre. All cameras showed sharp and tall light pillars extending out of every light source. Faint superparhelia were visible, too.

The crystal swarm was extending 3 km away from the centre itself. On the way there, upcoming cars spawned tall light pillars and visible parhelia.

Just as we arrived, the centre closed down and turned off the lights. We parked near the slope and noticed that it was completely overcast. The crystals were in the form of very thick fog that was hanging in the valley. More on the "weather side" later.

As we walked for a few hundred meters away from the centre, we stumbled upon a very bright lamp illuminating a local church. Only a sharp and tall light pillar was visible. But as we stayed for a little longer, the whole situation changed and superparhelia started to appear. At first they were hardly noticeable, but with each minute they were getting brighter and brighter.

We decided to try our not-so-much bright "spotlight" to see if anything interesting appeared. And yes it did. By shining the lamp towards the snowy surface, true divergence took form and divergent sub-parhelia appeared. They were eerily 3D, hanging in the air. Along with them, an extremely bright and tall light pillar was observed, too.

A multitude of light pillars


Tall light pillars and superparhelia


Circumzenithal arc along with light pillar and superparhelia 


Light pillar, sub-parhelia, parhelia, and parhelic circle

Now let's discuss the weather situation a little. The temperature reached below -16°C which was lower than other temperatures observed at meteorological stations (due to the topography). The ski centre was at the time actually located at the edge of a low hanging stratus that was just barely touching the mountain ridge. The snow guns then probably nucleated its lower layer and the crystals started to precipitate out. Below is a georeferenced image from the Suomi-NPP satellite along with the location of the centre. The microphysical product along with a high resolution of the image shows how the edge of a low stratus (yellow colour) extends towards our location. Now bare in mind that this image was taken approx. 1 hour after we left, so the stratus actually retreated a little by that time. There are two "branches" of a low stratus visible at the image. The right branch follows the exact location of a local dam called Šance. The left branch follows a river called Čeladenka.

(c) Suomi-NPP 24h microphysical product

What stuns me about this location is its abundance of diamond dust occurrences. Almost every time the snow guns are operating, a crystal swarm is created within minutes and light pillars are always visible on the webcam images. I have a theory about why that happens:
  • Microclimate - the topography is in the form of a depressed valley, which allows for a cool and moist air to accumulate at the bottom. 
  • Moisture - the river that flows through the village could possibly be a substantial source of moisture 
  • Snow gun additives - if I have learned well, it is the additives in the snow guns that serve as nuclei on which the crystal formation takes place. In that case, they are probably using a specific additive that makes the crystal formation so abundant. 
The local relief of Bílá
Shaded relief + topographic map
(c) ČÚZK


METAR analysis shows a high pressure centre located above Czechia
(c) METAR

Temperature distribution