Oxford MIPAS meeting#131
15 Jan 08

Present

Instrument Status [Prev] [Next]
Operating continuously since 1st Dec 2007 in standard cycle of 8 days NOM, 1 day MA, 1 day UA.
Currently in last day of NOM mode, MA mode tomorrow, etc
There are several unscheduled gaps in the L1B for December. Envisat web-site currently inaccessible so cannot access technical status reports which would normally explain some of them.

November Monthly Report [Prev] [Next]
November monthly report available on ESA web-site

L1B Data (JH) [Prev] [Next]
[L1B Data Coverage]
L1B coverage maps updated to Dec 30th
L1B data available on ESA server approximately 2 weeks after acquisition

Oxford L2 Processing (AD) [Prev] [Next]
Running MORSE to retrieve our own L2 data
Latest day processed: 28 Dec 2007
Processing all new data with a lag of around 2½ weeks (2 weeks for L1B data to appear, ~2-3 days process L2 locally)
Also processing all previous Oct/Nov/Dec data (2002-2006) in parallel to provide comparison with recent data
Some data recently supplied to EQUAL project (Envisat O3 and T validation)

Polar Stratospheric Clouds (JH) [Prev] [Next]
Trying to use SVD techniques to distinguish different types of PSC
  1. Found a good visual correlation between 1st three cloudy singular vectors and IMK Cloud-index method of classifying PSCs
  2. Also seems to be robust for different altitudes
  3. Now attempting to identify a suitable threshold for pairs of singular values to define PSC types.
  4. Next: process Antarctic winter of 2003 comparing SVD-derived PSC with IMK method.

Mesospheric Retrievals [Prev] [Next]
Found an efficient method for approximating the inverse of a large apodised noise covariance matrix.
Next step: find an efficient method for multiplying the large inverse covariance by the large transpose Jacobian (~10000 elements) when the noise varies slightly from scan to scan.

CO Retrievals (JW) [Prev] [Next]
Investigating how to incorporate non-LTE effects into a practical (i.e. near real time) operational scheme to retrieve CO

MIPAS - TES Radiance Comparisons (CW) [Prev] [Next]
Comparing MIPAS and TES limb-viewing radiances from 28 Jan 2005 (one of the few days when TES and MIPAS were both taking limb-view observations)

2007/8 Arctic Winter (AD) [Next]
From the [Recent Trend] plots of Oxford L2 data for Oct/Nov/Dec 10mb, averaged from 65N to 90N for 2007 (black) compared to recent years:

ACPD Papers [Prev] [Next]
Papers selected from the ACPD website for discussion
"Measurement of the water vapour vertical profile and of the Earth’s outgoing far infrared flux"
L. Palchetti et al. (published 10 Dec 2007, open until 04 Feb 2008)
Introduced by LMV.
"Inversion analysis of carbon monoxide emissions using data from the TES and MOPITT satellite instruments"
D. B. A. Jones et al (published 05 Dec 2007, open until 30 Jan 2008)
Comments being collected by JW
"Dependence of cloud fraction and cloud top height on surface temperature derived from spectrally resolved UV/vis satellite observations"
T. Wagner et al. (published 23 Nov 2007, open until 18 Jan 2008)
Comments being collected by JH
"Characterizing mega-city pollution with TES O3 and CO measurements"
C. Shim et al. (published 25 Oct 2007, open until 20 Dec 2007)
Comments were being collected by CW but discussion closed before anything was submitted.
Other MIPAS-related papers in the Open Discussion phase, which may be adopted at a future meeting
"Validation and data characteristics of methane and nitrous oxide profiles observed by MIPAS and processed with Version 4.61 algorithm"
S. Payan et al. (published 17 Dec 2007, open until 11 Feb 2008).
"Technical Note: Intercomparison of ILAS-II version 2 and 1.4 trace species with MIPAS-B measurements"
G. Wetzel et al. (published 22 Nov 2007, open until 17 Jan 2008)

Summary of MIPAS November Report

(text extracted from PDF document)

During the reporting month MIPAS performed really well; in fact only 2 instrument
anomalies occurred due to IDU errors (see §2.2.2).
• The instrument planning for the reporting month is hereafter summarized:
o The duty cycle was set to 80%
o The Baseline scenario was planned, it consists of the following measurements: 3
days NOM + 1 day MA + 1 day UA + 3 days NOM + 2 days off
• A more detailed description of the instrument planning for the reporting month can be found
in §2.2.1, see in particular Table 1.
• The availability of the instrument was high (97.8 % of the planned time) due to the good
performances of the interferometer. The measurement segments not processed to L0 due to
failures in the PDS were about 0.6% of the planned measurement time (see § 2.2.4).
• The long term analysis of L0 data availability shows the increased duty cycle since April
2006 and highlights the improved instrument performances in the last months (see §2.2.4.2).
• In this report we present the long term availability of L1 consolidated data in the D-PAC
server. We can see that the availability of L1 products with respect to the expected time is
approaching 100% in the last months (see §2.2.5).
• The instrument temperatures are stable over the reporting month, the variations being
included in 1K (see § 2.3.1).
• The cooler performs well during the reporting month; the vibrations were always well below
the warning level of 8 mg (see § 2.3.3).
• The long term trend of ADC max counts in channel A1 shows a strong correlation with the
instrument self-emission and with the detector ice contamination. During the reporting
month the ADC counts remain stable (see §2.3.4).
• The monitoring of the spectral correction factor shows a slight decreasing trend; however
the variations over more than two years of operations are really small (∼ 2 ppm). The
observed spreading of the points is due to the noise in the determination of this parameter
(see § 2.4.2).
• The gain weekly increase during the reporting month is nominal, the maximum of gain
increase in all the MIPAS bands remains well below the acceptance criterion of 1%/week
(see § 2.4.3.1).
• The analysis of the accumulated gain allows monitoring the level of detector ice
contamination. During the last months we observed a decreasing slope of the gain curve,
showing that the detector is more and more ice-free. This is due to the better performances
of the cooler obtained with more frequent decontamination (see §2.4.3.2).
• The absolute mispointing is stable around a value of -25mdeg. The seasonal variations of the
pointing error are small and below the fixed threshold of 8mdeg (see §2.4.4).
• The long term monitoring of fringe count errors (FCE) shows that the width of the statistical
distribution of the FCE can be used as a measure of the INT performances. In particular we
observed that the FCE can be correlated with the number of IDU errors. This correlation is
evident during the bad period of the MIPAS mission (June 2005 February 2006), while in
ENVISAT MIPAS Monthly Report: November 2007
issue 1 revision 0 - 15 Dec 2007
ENVI-SPPA-EOPG-TN-07-0078
page 5
the last months with the improved instrument performances no clear correlation can be
highlighted (see § 2.4.5.1).
• The long term monitoring of the detected spikes shows that the number of detected spikes in
channels A1, A2, B1 and B2 is varying with time with some peaks probably related to
variation of the solar activity. The channels C and D (the detector most affected by spikes)
didn’t show any trend so far. From this analysis we can conclude that the number of
detected spikes is still really small to impact the L1b products quality (see § 2.4.5.2).
• The level 0 NRT daily reports can be accessed at the following address:
http://earth.esa.int/pcs/envisat/mipas/reports/daily/Level_0_NRT/
• The level 1b OFL daily reports can be accessed at the following address:
http://earth.esa.int/pcs/envisat/mipas/reports/daily/Level_1_OFL/