On two potential sources of systematic error in

  • Slides: 27
Download presentation
On two potential sources of systematic error in retrievals using limb-scattered sunlight Chris A.

On two potential sources of systematic error in retrievals using limb-scattered sunlight Chris A. Mc. Linden (1) and Christopher E. Sioris (2) (1) Meteorological Service of Canada, Toronto, Ontario, Canada (chris. mclinden@ec. gc. ca) (2) Atomic and Molecular Physics Division, Harvard. Smithsonian Center for Astrophysics, Cambridge, Massachusetts, USA 14 -16 April 2003 International Limb Workshop, Bremen

Outline 1. Allowing for a varying atmosphere along the line-of-sight (LOS) when performing retrievals

Outline 1. Allowing for a varying atmosphere along the line-of-sight (LOS) when performing retrievals 2. Systematic errors in plane-parallel models, including so-called “pseudospherical” limb scattering models. 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (1) w Perform multiple plane-parallel calculations, each one for

Varying atmosphere along the LOS (1) w Perform multiple plane-parallel calculations, each one for a particular atmosphere & SZA along the LOS w From these, calculate LOS sources function – integrate to obtain limb radiance w Using vector RT model of Mc. Linden et al. (Can. J. Phys. , 80, 375 -383, 2002) 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (2) - in practice, slices narrower near tangent point

Varying atmosphere along the LOS (2) - in practice, slices narrower near tangent point 2 N 14 -16 April 2003 1 International Limb Workshop, Bremen OS or SCIA

Varying atmosphere along the LOS (3) w Want to estimate magnitude of errors when

Varying atmosphere along the LOS (3) w Want to estimate magnitude of errors when atmosphere is not homogeneous along LOS, but assumed to be in retrieval (‘ 2 D’ forward, ‘ 1 D’ inversion) w If species diurnal, can a ‘ 2 D’ retrieval improve result for scans near terminator and SZA variations along LOS ? 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (4) 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (4) 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (4) - Flittner algorithm used -‘ 2 D’ forward

Varying atmosphere along the LOS (4) - Flittner algorithm used -‘ 2 D’ forward calculation, ‘ 1 D’ inversion 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (5) 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (5) 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (6) -Sioris NO 2 inversion algorithm used -Uses an

Varying atmosphere along the LOS (6) -Sioris NO 2 inversion algorithm used -Uses an iterative onion peel technique SZA=27º, d. AZ=92º; Aug. , 25ºN, albedo=0 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (7) SZA=27º, d. AZ=92º; Aug. , 25ºN, albedo=0 14

Varying atmosphere along the LOS (7) SZA=27º, d. AZ=92º; Aug. , 25ºN, albedo=0 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (8) SZA=27º, d. AZ=92º; Aug. , 25ºN, albedo=0 14

Varying atmosphere along the LOS (8) SZA=27º, d. AZ=92º; Aug. , 25ºN, albedo=0 14 -16 April 2003 International Limb Workshop, Bremen

Varying atmosphere along the LOS (9) Comparison of ‘ 1 D’ and ‘ 2

Varying atmosphere along the LOS (9) Comparison of ‘ 1 D’ and ‘ 2 D’ OSIRIS inversions with HALOE coincidence LOS scaling factors from photochemical box model 4 June 2002 lat=4ºN, lon=55ºW 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (1) - Comparison of several “pseudo-spherical” (PS)

Systematic Errors in “Pseudo. Spherical” Limb Radiances (1) - Comparison of several “pseudo-spherical” (PS) radiative transfer model calculations with 3 -D, spherical Monte-Carlo (MC) model calculations show systematic errors - These errors increase with (a) tangent height and (b) surface albedo 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (2) SZA=39º; albedo=0. 95 14 -16 April

Systematic Errors in “Pseudo. Spherical” Limb Radiances (2) SZA=39º; albedo=0. 95 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (3) -PS calculations based on plane-parallel source

Systematic Errors in “Pseudo. Spherical” Limb Radiances (3) -PS calculations based on plane-parallel source function & integrated through spherical-shell atmosphere -These errors are driven by an overestimation of the surface reflected component – either the surface proper or the effective Rayleigh “surface” 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (4) -root of problem is how much

Systematic Errors in “Pseudo. Spherical” Limb Radiances (4) -root of problem is how much of the surface a point in the atmosphere “sees”: -PP atmosphere: point sees 2 [str] -spherical atmosphere: point sees <2 [str]; this decreases with altitude 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (5) Direct Point under consideration Surface reflected

Systematic Errors in “Pseudo. Spherical” Limb Radiances (5) Direct Point under consideration Surface reflected 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (6) - try simple, near-transparent atmosphere correction

Systematic Errors in “Pseudo. Spherical” Limb Radiances (6) - try simple, near-transparent atmosphere correction factor using ratio of PS to spherical solid angles Where 14 -16 April 2003 is cos(SZA) and is surface albedo International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (7) 800 nm SZA=39º 14 -16 April

Systematic Errors in “Pseudo. Spherical” Limb Radiances (7) 800 nm SZA=39º 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (8) -Trace gas retrievals should be minimally

Systematic Errors in “Pseudo. Spherical” Limb Radiances (8) -Trace gas retrievals should be minimally impacted since there will be cancellation/removal of this effect - e. g. , the Flittner radiance-ratio method there will be a large degree of cancellation due to form of retrieval vector; - in DOAS it will not cancel but it would be included or removed in closure polynomial or high pass filter 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (9) -Aerosol retrievals may suffer systematic errors

Systematic Errors in “Pseudo. Spherical” Limb Radiances (9) -Aerosol retrievals may suffer systematic errors if the retrieval involves a modelmeasurement matching of radiances -If aerosol signal small, the PP errors can lead to amplified aerosol errors; unclear how “optimal”-type solutions would handle this 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (10) -If aerosol signal is: S =

Systematic Errors in “Pseudo. Spherical” Limb Radiances (10) -If aerosol signal is: S = I(measure) – I(model w/o aerosol) -But P-P aerosol signal is: SPP = I(measure) – I(model w/o aerosol) / c Where c= 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances 14 -16 April 2003 International Limb Workshop,

Systematic Errors in “Pseudo. Spherical” Limb Radiances 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (12) 14 -16 April 2003 International Limb

Systematic Errors in “Pseudo. Spherical” Limb Radiances (12) 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (13) 14 -16 April 2003 International Limb

Systematic Errors in “Pseudo. Spherical” Limb Radiances (13) 14 -16 April 2003 International Limb Workshop, Bremen

Conclusions & Future Work -systematic PS errors may be important in OS aerosol retrievals

Conclusions & Future Work -systematic PS errors may be important in OS aerosol retrievals + other RT applications including photochemistry (& other planetary atmospheres) -attempt to obtain “universal” correction valid at all wavelengths, tangent heights, albedo 14 -16 April 2003 International Limb Workshop, Bremen

Systematic Errors in “Pseudo. Spherical” Limb Radiances (14) 14 -16 April 2003 International Limb

Systematic Errors in “Pseudo. Spherical” Limb Radiances (14) 14 -16 April 2003 International Limb Workshop, Bremen