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An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar 9 August 2007

An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

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Page 1: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

An ultra-Narrowband Magneto-Optical Filter

for Daylight Observations of the

Mesospheric Potassium Layer

An ultra-Narrowband Magneto-Optical Filter

for Daylight Observations of the

Mesospheric Potassium Layer

Jonathan S. FriedmanArecibo Observatory Seminar

9 August 2007

Jonathan S. FriedmanArecibo Observatory Seminar

9 August 2007

Page 2: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Arecibo Observatory, 9 August 2007

Page 3: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Arecibo Observatory, 9 August 2007

The solar spectrum near the K D-lines is heavily populated with O2 rotational absorption lines. In fact, the D2 line in potassium overlaps one such line.

The solar spectrum near the K D-lines is heavily populated with O2 rotational absorption lines. In fact, the D2 line in potassium overlaps one such line.

Potassium has coronal absorption bands, i.e. Fraunhofer lines. The D1 Fraunhofer absorption is shown at right.

Potassium has coronal absorption bands, i.e. Fraunhofer lines. The D1 Fraunhofer absorption is shown at right.

Page 4: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Spectral FilteringSpectral Filtering

Arecibo Observatory, 9 August 2007

• There are a variety of methods of spectral filtering. Color filters, spectrometers/monochrometers, interference filters and etalons are the most common.

• These suffer from low line-center throughput, broad bandwidth, poor spectral discrimination, and/or high cost. Etalons are the only technology that can work in daylight. • Etalons suffer from high cost + stability problems, especially when multiple etalons are required.

Page 5: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Advantages of the Faraday Anomalous Advantages of the Faraday Anomalous Dispersion Optical FilterDispersion Optical Filter

Advantages of the Faraday Anomalous Advantages of the Faraday Anomalous Dispersion Optical FilterDispersion Optical Filter

Arecibo Observatory, 9 August 2007

• Adjustable-width, ultra-narrowband optical filtering.

• Flat-topped filter

• No wavelength drift

•Low cost ($20K) vs. multiple etalons (>$50K)

Page 6: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

What is a Faraday Filter? (AKA Magneto-What is a Faraday Filter? (AKA Magneto-Optical Filter or FADOF)Optical Filter or FADOF)

What is a Faraday Filter? (AKA Magneto-What is a Faraday Filter? (AKA Magneto-Optical Filter or FADOF)Optical Filter or FADOF)

The Faraday filter uses an atomic vapor cell in an axial magnetic field to rotate the polarization of light that is resonant with an electronic transition of the atomic species that makes up the vapor.

The cell and B-field are sandwiched between crossed polarizers, so light that is not resonant, and passes unimpeded through the cell does not have its polarization rotated and is extinguished.

Arecibo Observatory, 9 August 2007

Page 7: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Arecibo Observatory, 9 August 2007

Page 8: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Physical Principles (continued)Modeling the Faraday Filter

Physical Principles (continued)Modeling the Faraday Filter

Arecibo Observatory, 9 August 2007

QuickTime™ and aVideo decompressor

are needed to see this picture.

Page 9: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

The AO FADOF and its spectral effectThe AO FADOF and its spectral effect

Arecibo Observatory, 9 August 2007

Page 10: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

A FADOF can also be used for Rayleigh Wind Lidar

Arecibo Observatory, 9 August 2007

Page 11: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

The Arecibo FADOF DesignThe Arecibo FADOF Design

Arecibo Observatory, 9 August 2007

Page 12: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Performance Tests (for 1 channel)

Arecibo Observatory, 9 August 2007

Performance Tests (for 2 channels)

Page 13: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

K FADOF performance at Tenerife (28°N, 16.5° W)

K FADOF performance at Tenerife (28°N, 16.5° W)

Arecibo Observatory, 9 August 2007

Page 14: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

SummarySummary

Understanding of the MLT region requires round-the-clock observations of state variables.

The solar background is obviously a huge problem for optical observations.

There are not many useful technologies, and most are costly and unwieldy.

The FADOF resolves many issues, providing a useful, economical, efficient and stable means of reducing the solar background with high line-center throughput.

Understanding of the MLT region requires round-the-clock observations of state variables.

The solar background is obviously a huge problem for optical observations.

There are not many useful technologies, and most are costly and unwieldy.

The FADOF resolves many issues, providing a useful, economical, efficient and stable means of reducing the solar background with high line-center throughput.

Arecibo Observatory, 9 August 2007

Page 15: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Extra Slides

Page 16: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

K Energy Level DiagramK Energy Level Diagram

Page 17: An ultra-Narrowband Magneto-Optical Filter for Daylight Observations of the Mesospheric Potassium Layer Jonathan S. Friedman Arecibo Observatory Seminar

Filter curve for 2-pass Version

Normalized Normalized transmissions of transmissions of emissions due to emissions due to the three laser the three laser wavelengths:wavelengths:0.98440.98440.98440.98440.98450.9845