Monthly Mean data for September 2003 now plotted
(excludes 8-19 Sep when there were gain calibration
problems)
- Altitude (AD)
- Changes from previous month generally <100m
- Temperature (AD)
- S.Polar and Mid Latitude regions warming by up to 10K compared to
previous month below 50km,
cooling above.
- N.Polar region cooling by up to 10K compared to previous month
- Low latitude profiles continue approx 10K cooler than initial guess
climatology at 40km
- Pressure (AD)
- N.hemisphere and equatorial pressures reduced by 10-20%
compared to previous month
- S.Polar pressures increased by 10-15% above 21km, reduced by a few
% below
- S.Mid Latitude pressures increased by a few % above 36km, reduced
by up to 10% below
- Pressure in polar regions now departs from IG climatology by >40%
at high altitudes (S.Polar is lower, N.Polar is higher),
while converging to within 10% for other latitudes
- CH4 (VP)
- The equatorial profiles show a strange shape,
with a local minimum at 15km.
This has been the case since July.
(From January to June, there was a strange minimum visible at
18km).
- It was suggested that the change in
this feature could have been brought about by the implementation of cloud
detection in the processor in July(?).
- Values in the northern
mid-latitude and polar profiles are slightly lower than last month.
- H2O (VP)
- The southern polar profile is a strange shape, being around 1.2ppmv
lower than the IG profile at 18km. However, the shape is consistent with
last month's profile.
- It was suggested that this may be due to
dehydration within the polar vortex.
- 2CH4+H2O (VP)
- Profiles of this quantity are somewhat higher than would be
expected from climatology (around 1ppmv upwards of 21km).
- This is in
keeping with profiles from previous months.
- HNO3 (AD)
- Equatorial latitudes identical to August, and lower than the
climatology.
- N.Hem Polar and Mid Lat values greater than previous month,
S.Hem Polar and Mid Lat less than previous month.
- The S.Polar values above 30km are much less than the IG climatology
- N2O (AB)
-
The mean is very similar to August, where the 12km altitude (especially at
the equator) is much larger than climatology at 500-700 ppbv vs 300ppbv.
- The poles are lower than before, and have a higher variability.
- There is persistent structure at 21km, S.Polar latitudes,
not much stronger than last month.
- Persistent enhancements at 12km, Equ-20N.
- NO2 (AD)
- S.Polar nighttime max reduced in altitude compared to
previous month (30km
instead of 36-42km
- Other latitudes have nighttime peak values between 33-39km
- N.Polar nighttime profile increasing, daytime profile decreasing
- No significant change at other latitudes
- O3 (AD)
- N.Polar latitudes decreasing by 5-10% compared with previous month,
S.Mid latitudes increasing by 5-10%, no significant change at other latitudes
- Values continue to exceed IG climatology by 1ppmv at 40km at all
latitudes
- S.Hem values continue 0.5ppmv lower than climatology at 21-24km
ASSFTS-11 Workshop (8-10th Oct, Bad Wildbad, Germany)
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Some notes on presentations
- Radiometric Characterisation of MIPAS/Envisat (Manfred Birk, DLR)
- Estimates errors of up to 5% (for low radiances)
from non-linearity correction
- 135Hz pointing jitter may lead to ghost spectra +/-
13cm-1 of 1.8% amplitude - origin from Stirling cooler?
- Microvibrations also lead to ghost spectra <1% amplitude.
- Study of Trade-Off between accuracy and horizontal resolution
(Marco Ridolfi, IFAC)
- With nominal scan can retrieve 2 profiles per scan (250km spacing)
with SD increased by a factor 2
- With 0.1cm-1 spectral resolution (1/4 OPD) can retrieve
at 133km horizontal spacing.
- Retrieval of temperature and pointing information from MIPAS limb
emission specta (Thomas von Clarmann, IMK)
- IMK use fixed 1km altitude grid for retrievals, which simplifies
ray-tracing and FOV convolution during pT retrieval iterations
- Noted 3km jump in reported tangent altitudes in early MIPAS data
when new orbital parameters uploaded
- MIPAS L2 Near Real Time processor performance (Piera Raspollini,
IFAC)
- ILS correction expected to induce a negative shift of 50-100m in
pointing
- Offline processor includes new convergence criteria and extended
altitude range - requires approx. 2x CPU of NRT.
- Tested with orbits 2994 (26Sep02) and 8225 (26Sep03)
- MIPAS measurements of ClONO2 and PSCs during the Antarctic Vortex
Split in September 2002 (Michael Hoepfner, IMK)
- Only processed data from 18Sep02 onwards, problems with earlier data
(unstable temperature retrievals)
- Using Wagner & Birk (2003) ClONO2 cross-section data
- CH4 and N2O sysematically higher in Sep02 than Oct02
- Also retrieving ClO
- Non-LTE Retrieval of NO, NO2 and CO from MIPAS-Envisat (Bernd Funke,
IAA/IMK)
- Jul and Sep 02 data, retrieved at 10-15km vertical resolution
- Non-LTE model included as part of retrieval forward model
- NO includes rotational non-LTE
- NO2 only significant non-LTE effects during polar winter
- Use SPIRALE CO and HALOE NO+NO2 for validation
- Validation of MIPAS operational L2 products using ground-based
network data (Martine de Maziere, BIRA)
- Comparison with O3 measurements from Payerne show that v4.55
was worse than v4.53 (Dec02) (version history)
- NO2: v4.55 and v4.57 appear to have more scatter than v4.53.
Oxford/RAL posters & presentations