This is an image of clouds taken from the top of the Regent Parking structure on the CU main campus on 10/8/19 around 3:00pm. According to the Skew T Diagram (see above PDF), the main cloud in the photo is altocumulus with some altostatus surround them at about an altitude of 5600m. This is an unstable environment since it was the day before a large snow storm. Shot with IPhone 6, f/2.2, 1/15385sec, ISO 25, FL: 4mm.
Jason Fontillas // Clouds 1
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Flow Vis Guidebook
- Introduction to the Guidebook
- Overview 1: Phenomena. Why Does It Look Like That?
- Overview 2: Visualization Techniques
- Overview 3: Lighting
- Overview 4 - Photography A: Composition and Studio Workflow
- Overview 4 - Photography B: Cameras
- Overview 4 - Photography C: Lenses - Focal Length
- Overview 4 - Photography C: Lenses - Aperture and DOF
- Overview 4: Photography D: Exposure
- Overview 4 - Photography E - Resolution
- Overview 5 - Post-Processing
- Clouds 1: Names
- Clouds 2: Why Are There Clouds? Lift Mechanism 1: Instability
- Clouds 3: Skew - T and Instability
- Clouds 4: Clouds in Unstable Atmosphere
- Clouds 5: Lift Mechanism 2 - Orographics
- Clouds 6: Lift Mechanism 3 - Weather Systems
- Boundary Techniques - Introduction
- Dye Techniques 1 - Do Not Disturb
- Dye Techniques 2 - High Visibility
- Dye Techniques 3 - Light Emitting Fluids
- Refractive Index Techniques 1: Liquid Surfaces
- Refractive Index Techniques 2: Shadowgraphy and Schlieren
- Particle Physics: Flow and Light
- Dilute Particle Techniques - Under Construction
- Particles 2: Aerosols
- Particles 3: In Water - Under Construction
- Art and Science
- TOC and Zotpress test
- Photons, Wavelength and Color
3 Comments. Leave new
The morning CAPE was zero, as Brian Gomez’ skew-T shows. I think the front arrived a bit later, so I’d call these Mountain wave clouds below cirrus.
The contrast on the photo is brilliant. I really enjoy the layers of the clouds
The different layers of light and dark are amazing. It looks like a painting.