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EGS-AGU-EUG Joint Assembly, Session AS27, Nice 6-11 April 2003

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Presentation on theme: "EGS-AGU-EUG Joint Assembly, Session AS27, Nice 6-11 April 2003"— Presentation transcript:

1 EGS-AGU-EUG Joint Assembly, Session AS27, Nice 6-11 April 2003
Page 1 EGS-AGU-EUG Joint Assembly, Session AS27, Nice 6-11 April 2003 A survey of non-LTE atmospheric emissions as measured by MIPAS/Envisat M. López-Puertas for the IMK-IAA MIPAS Group: B. Funke, M. García-Comas, S. Gil-López, M. López-Puertas, M.Á. López-Valverde (IAA, Granada) T. von Clarmann, H. Fischer, N. Glatthor, U. Grabowski, M. Höpfner, S. Kellmann, M. Kiefer, A. Linden, G. Mengistu Tsidu, M. Milz, T. Steck, G.P. Stiller, D.Y. Wang (IMK, Karlsruhe)

2 Contents Introduction
Some "first-detected" NLTE emissions obverved by MIPAS Retrievals of NLTE parameters (CO2 4.3 µm, NO2 chem. exc.) Retrievals of pressure/temperature and vmrs under NLTE Pressure-Temperature Ozone, NO, NO2, CO Conclusions

3 Introduction Unprecedented data measured by MIPAS for non-LTE studies:  Spectra of high resolution (0.035 cm-1) and wide coverage ( µm)  High sensitivity (30-3 nW/(cm2 sr cm-1))  Global spatial (pole-to pole) and temporal (day and night) coverages. Two approaches:  Analysis of spectra for gaining new non-LTE information  Retrievals of geophysical parameters which required non-LTE (known) Data used:  Nominal MIPAS mode: 3 km, 47, 52, 60, 68 km  Upper Atmosphere mode (5 orbits, 1 Jul 2002): km.

4 MIPAS spectra, Band A, Th 68 km
Night Day Non-LTE CO2 10µm laser emissions Warmer nighttime temperatures

5 MIPAS upper atmosphere data Orbits 1748-52. 1 July 2002

6 NLTE Daytime enhancement in CO2 15µm
% cm-1

7 MIPAS spectra, Band AB, Th 68 km
Night Day O Non-LTE CO2 10µm laser band O3 9.6 µm ( )

8 MIPAS spectra, Band B, Th=66 km
Night Day

9 NLTE in CH4,TH=66 km Day SH Day NH Night

10 NLTE Daytime enhancement in CH4
cm-1 %

11 MIPAS spectra, Band C, Th=30 km
Night Day Signal larger at night because NO2 is larger

12 Retrieval of NO2 chem exct. rate
Orbit 2108 (24 July)

13 MIPAS spectra, Band C, Th 68 km
Night Day H2O HOT band lines

14 MIPAS spectra, Band C, Th 68 km, H2O FH
Night Day H2O fundamental band lines H2O HOT band lines

15 NLTE Daytime enhancement in H2O
% (D+N) cm-1

16 MIPAS spectra, Band D, Th 68 km
Night Day CO2 NO CO

17 MIPAS spectra, Band D, Th 68 km, NO
- Rotational and spin nitric oxide lines resolved. - Larger at daytime, as expected - Most of radiation coming from the thermosphere Night Day

18 Band D, Th=101 km, NO 5.3µm hot band
Night Day NO(2-1) NO(2-1)

19 O3(102001) HB at 56 km Night Day SH DAY NH

20 Band D, Th 68 km, CO Night Day

21 CO(21) hot band at 71 km Night Day

22 OH(98) emission -------- Night, 76km -------- Night, 81km

23 Band D, Th=68 km, CO2 4.3 µm CO2 hot (mainly) and fundamental (small) bands CO2 fundamental band CO2, 636- isotope lines

24 CO2 collisional rates in the 2.7µm levels
SH3 SH2 FB 628 FH SH1 626 636

25 The Non-LTE retrieval scheme (1)
Jointly developed IMK-IAA non-LTE processor for retrievals of p-T, vmr's, and NLTE parameters.

26 The Non-LTE retrieval scheme (2)
Optimization algorithm Iterative constrained nonlinear least squares global fit Regularisation: Tikhonov smoothing (Temperature, vmr's) Optimal estimation (LOS and CO2) Forward model: KOPRA Line-by-line radiative transfer model Interface for NLTE-model Computes spectra and Jacobians for LTE and non-LTE

27 The Non-LTE retrieval scheme (3)
The non-LTE model: the Generic RAdiative traNsfer AnD non-LTE population Algorithm (GRANADA) Calculation of vibrational populations, and their derivitavies w.r.t the NLTE retrieval parameters Generic: same algorithm used for calculating non-LTE populations of different gases (CO2,O3, CO, NO, NO2, H2O, OH, etc.) Very flexible. User defines the energy levels and transitions, iteration strategies, process definition, etc. Rotational (and spin-orbit) non-LTE Line-by-line and line independent radiative transfer (KOPRA) Inversion of multilevel steady state equation by using Lambda iteration or Curtis matrix formalism Interface module to forward model

28 Pressure-temperature in the upper atmosphere
1 July 2002, Orbit 1750 NP Eq SP Eq NP

29 CO2 vmr in the upper atmosphere
1 July 2002 Orbit 1750 NP Eq

30 O3 vmr in the stratosphere and mesosphere (2)
NIGHTTIME DAYTIME 1 July 2002, Orbits

31 O3 vmr in the stratosphere and mesosphere (1)
1 July 2002, Orbit 1750 NIGHT 86ºS DAY 78ºN O3 tertiary max.

32 CO vmr in the stratosphere and mesosphere
1 July 2002, Orbit 1748 Eq SP Eq NP Eq

33 Nitric Oxide (NO) 1 July 2002, Orbit 1748 Eq SP Eq NP Eq

34 NO2 1 July 2002, Orbit 1748 Eq SP Eq NP Eq

35 Conclusions MIPAS measurements are an unprecendent dataset for improving our knowledge of non-LTE processes in the atmopshere By including non-LTE, we have been able to retrieve many geophysical parameters (p-T, O3, CO2, CO, NO, NO2, H2O, CH4) from the stratosphere up to the lower thermosphere

36 End of Presentation


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