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ATBD - GHG-CCI

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ESA Climate Change Initiative (<strong>CCI</strong>)<br />

Algorithm Theoretical Basis Document<br />

Version 2 (<strong>ATBD</strong>v2) – UoL-FP<br />

for the Essential Climate Variable (ECV)<br />

Greenhouse Gases (<strong>GHG</strong>)<br />

Page 23<br />

Version 2 – Draft 1<br />

18 March 2013<br />

3.4 Screening<br />

3.4.1 Pre-Processing Screen<br />

The GOSAT L1B soundings are screened initially to filter out any observations where the<br />

signal to noise (SNR) is < 50, if the sounding is over ocean and if a sounding contains any<br />

invalid L1B data.<br />

3.4.2 Cloud Screen<br />

One major disadvantage of using SWIR observations is that the iFOV must be free of thick<br />

clouds as these will cause irradiation to be reflected towards the satellite from a higher<br />

altitude, that of the cloud, rather than the Earth's surface. Therefore, a cloud screen is<br />

necessary to filter out exposures where thick clouds are within the iFOV. When irradiation<br />

gets reflected towards the satellite from a thick cloud the effective surface is that of the cloud<br />

rather than the Earth's surface. This results in the actual surface pressure being that at the<br />

cloud altitude, which typically is significantly lower than that at the Earth's surface pressure.<br />

An estimate of the actual surface pressure can be obtained by performing O 2 A band<br />

retrievals where the surface pressure is retrieved. We implement a super fast O 2 retrieval by<br />

using a small spectral window (13056 to 13074.8 cm -1 ). If the retrieved surface pressure is<br />

compared to the a priori surface pressure then the difference in surface pressure can be<br />

determined. Since the a priori surface pressure is well constrained, a surface pressure<br />

difference of greater than 30 hPa would normally only occur if a thick cloud is present in the<br />

iFOV, thus the exposures can be cloud screened using this method.<br />

3.4.3 Post-Processing Screen<br />

3.4.3.1 Carbon Dioxide Screen<br />

The CO 2 is post-screened based on the algorithm convergence criteria as above (i.e.<br />

outcome =1 or 2) as well as on the normalised CHI-Squared value for each spectral band.<br />

Currently a threshold of 0 < CHI-Square Band 1 < 1.3, 0.6 < CHI-Square Band 2 < 1.5 and<br />

0.4 < CHI-Square Band 3 < 1.5 is used. In addition to these screens we also presently filter<br />

on a number of other parameters to reduce the<br />

Additionally, these full physics retrievals are subjected to spectral interference from aerosols<br />

and clouds and topographic assumptions of the a priori, therefore we apply a number of<br />

extra screens to reduce these effects as explained in the table below.<br />

Table 3-4. Description of additional parameters used in the Carbon Dioxide post-processing<br />

screen.<br />

Parameter<br />

Minimum<br />

Threshold<br />

Maximum<br />

Threshold<br />

Explanation<br />

Saturation Test Band 2<br />

Polarisation P<br />

0 3.5x10 -5 Instrument saturation Flag determined from L1B<br />

radiance.

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