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Thursday, November 26, 2015

Double Rainbow Astrophotography Zion National Park

During my trip to Zion National Park, the weather was far from ideal for astrophotography. Clouds moved quickly across the sky, rain showers passed through the canyon, and the night sky remained hidden.

But sometimes nature offers something unexpected.

After one of the storms, sunlight broke through the clouds and illuminated the moist desert air. What followed was spectacular — a double rainbow stretching above the dramatic sandstone cliffs of Zion.

It made me pause and think: Is a rainbow astrophotography?

Technically, a rainbow is an optical atmospheric phenomenon caused by the interaction of sunlight with water droplets. The Sun — our nearest star — provides the light source. In that sense, this image captures a phenomenon directly created by astronomical light interacting with Earth's atmosphere.

So while it may not show stars, planets, or the Milky Way, it still documents a beautiful example of astronomy meeting atmospheric physics.


 
Double rainbow over Zion National Park after desert rain storm with sandstone cliffs illuminated by sunlight
Double Rainbow Astrophotography Zion National Park

Why Does a Double Rainbow Happen?

A primary rainbow forms when sunlight enters a raindrop, bends (refracts), reflects once inside the droplet, and exits — separating into colors.

A secondary rainbow appears when light reflects twice inside the droplet before exiting. This second internal reflection causes:

  • Reversed color order (red on the inside, violet on the outside)
  • A fainter and wider outer arc
  • A darker region between the two rainbows known as Alexander’s Band

Double rainbows are less common because they require:

  • Strong, low-angle sunlight (often late afternoon)
  • Large numbers of evenly distributed raindrops
  • The observer positioned with the Sun behind them

In desert environments like Zion, storms can be brief but intense — creating perfect conditions when sunlight returns.

Even though this was not the astrophotography session I had planned, this moment reminded me that sky photography is not limited to night. Sometimes the most powerful celestial light comes from the Sun itself.

Related Astrophotography & Sky Phenomena Posts

These posts explore how celestial light interacts with Earth’s atmosphere and environment — from atmospheric optics to interplanetary dust and extreme dark-sky effects.

Sunday, November 15, 2015

Orion (constellation) Astrophotography

His head is made of stars, but not yet arranged into constellations. 

-- Elias Canetti


One of the most recognizable constellations in the sky is Orion. There is my collection of Orion astrophotography from different counties. 

Orion Constellation Astrophotography Israel
Orion Constellation Astrophotography Culebra Island Puerto Rico


Orion Constellation and Northern Light Island Astrophotography

Orion Nebula M42 Urban NYC Astrophotography

Orion Constellation Astrophotography
Constellation Orion Israel Astrophotography from Kfar Szold Kibbutz

Constellation Orion Astrophotography Puerto Rico

Friday, November 6, 2015

Green Sky Utah Airglow Astrophotography Canon 60Da

The sky is green, the night is dark - as simple as possible. This photo was done at Bryce Canyon, Utah. Canon 60Da, EF16-35mm f/2.8L II USM, 30.0 sec; f/3.5; ISO 6400

Green Sky Utah Airglow Astrophotography Canon 60Da
The natural moonless night sky is dark but not black; it is not even blue (no scattering light from sun and moon). Earth atmosphere  emits green, red, orange, yellow light- Airglow!

About 60% of the natural brightness of the night sky at zenith is made up of Airglow. Maximum brightest usually appears at about 10-15 degrees above the horizon, because of the greater the depth of atmosphere at this angle. Airglow is not always uniform. Gravity waves may create considerable variation of Airglow brightness.

You can see Airglow only in real dark sky, but naked eye could not recognize colors. Photos with long exposure able get the colors of Airglow.

The usually dominant color of airglow is green originated from molecular oxygen at 90 to 100 km high. Orange and reddish hue caused by atomic oxygen in 150-300 km above the ground, Yellow light comes from sodium atoms in a layer at about 90 km.