Neutral Atmosphere and Geodesy - TU Wien · 2015-08-17 · • Atmospheric corrections as...
Transcript of Neutral Atmosphere and Geodesy - TU Wien · 2015-08-17 · • Atmospheric corrections as...
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Johannes Böhm
Neutral Atmosphere and Geodesy
Acknowledgement: Gregor Möller, Michael Schindelegger, ..
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The Atmosphere ...
• .. does not only cause troubles ..
• .. but opens a wide range of possibilities for geodesy
2 wikipedia.org
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The Atmosphere ...
.. delays signals in the • ionosphere and • troposphere,
.. influences • Earth rotation, • satellite orbits, • Earth gravity field
3 wikipedia.org
.. moves points due to • loading and • thermal deformation.
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The Atmosphere ...
4 wikipedia.org
.. delays signals in the • ionosphere and • troposphere,
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Refractivity N = N (p, T, e)
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[Nilsson et al., 2013]
liquid water
1013 hPa, 300 K, 100%
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Troposphere Delays
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Troposphere Delays
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[Nilsson et al., 2013]
[Saastamoinen, 1972; Davis et al., 1985]
estimated
Vienna
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Pressure Values
• Observed values – at epoch
• Numerical weather models – every 6 hours
• Blind models – Berg (1948) – Hopfield (1969) – UNB3m, GPT2, ...
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3 hPa → 1 mm height
O'Higgins, Antarctica
destructive effect of blind models with loading
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e
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Mapping Functions
Partials Clocks 1 Height sin(e) Zenith delay ≈ mf(e)
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e
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Mapping Functions
Partials Clocks 1 Height sin(e) Zenith delay ≈ mf(e)
5 mm @ 5° elevation → 1 mm height
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Mapping Functions
• Niell Mapping Functions – blind
• Isobaric Mapping Functions • Vienna Mapping Functions 1
– ECMWF analysis (6 h) • Global Mapping Functions
– ‘averaged VMF1’ – blind – GPT2
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Fortaleza (Brazil)
hydr
. mf a
t e =
5°
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GPT2 and GPT2w
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GPT2 GPT2w amendments
2001-2010 monthly mean profiles from ERA-Interim (37 levels) -
5° grid at mean ETOPO5 heights 1° grid
Mean, annual, semi-annual terms; phases estimated -
Pressure, temperature, water vapour pressure, lapse rate and mapping function coefficients
mean temperature Tm and water vapour decrease factor λ
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Blind Model for ∆Lwz: GPT2w
• Water vapour decrease factor λ estimated from ray-traced zenith wet delay
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( ) m
sd
m
zw g
eRTkkL
110 3'
26
+
+=∆ −
λ
∫∫∞
∞
=
H
Hm
zTe
zTeT
d/
d/2
( ) 1+= λss ppee
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Blind Model for ∆Lwz: GPT2w
• Water vapour decrease factor λ estimated from ray-traced zenith wet delay
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λ semi-annual amplitude []
( ) 1+= λss ppee
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Blind Model: GPT2w
• RMS differences w.r.t. IGS ZTDs about 3.4 cm on average
18 RMS differences in cm over 2012
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Ray-tracing
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• Great potential but limitations with large number of GNSS observations
• Many active groups, e.g., – GSFC, UNB, NICT, GFZ, GRGS,
Vienna, ... • GSFC has shown improvement for
VLBI baseline length repeatabilities
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GNSS Meteorology
• Ground based – precipitable water, tomography
• Space based – radio occulation
• Climate monitoring
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mm
Nilsson, 2011
Wettzell
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The Atmosphere ...
.. delays signals in the • ionosphere and • troposphere,
.. influences • Earth rotation, • satellite orbits, • Earth gravity field
21 wikipedia.org
.. moves points due to • loading and • thermal deformation.
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Angular Momentum vs. Torque Approach
(1) Conservation of angular momentum in total system (solid Earth + fluids)
(2) Torque approach considers fluids as external layers:
“push-and-pull” interaction with solid Earth
Atmosphere
Pole
Change in fluid angular momentum
[Schindelegger, 2014]
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Torque Approach
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Gravitation Friction
Pressure
Total torque of solid Earth (s) on the atmosphere (a)
fmesaas LLLLL ++=−= →→ )()()()(
Ellipsoidal torque Mountain torque Friction torque
Local Torques
0p pp ∆+0
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Geophysical Influences on LOD
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[Schindelegger, 2014]
LOD:
cha
nges
in le
ngth
-of-d
ay
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Mass (pressure) or motion (wind) terms?
Geophysical Influences on LOD
puga
volume
dddcos 23
φλφ∫∫∫φλφ ddcos34
∫∫surface
spga
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Atmospheric Excitation of Earth Rotation Important ..
• .. for a better understanding of the system Earth • E.g., prograde annual nutation
27 Michael Schindelegger
VLBI residual
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Atmospheric Excitation of Earth Rotation Important ..
• .. for a better understanding of the system Earth • .. as boundary condition for NWMs • Predictions of Earth rotation based on NWM forecasts
are of importance for spacecraft tracking (0.1 ms = 1.6 km @ Mars) and real time GNSS orbits
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The Atmosphere ...
.. delays signals in the • ionosphere and • troposphere,
.. influences • Earth rotation, • satellite orbits, • Earth gravity field
29 wikipedia.org
.. moves points due to • loading and • thermal deformation.
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Atmospheric Effects on the Earth Gravity Field
• De-aliasing products for CHAMP, GRACE, GOCE • .. for an improved detection of hydrology
30 wikipedia.org
pressure geoid
Maria Karbon
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The Atmosphere ...
.. delays signals in the • ionosphere and • troposphere,
.. influences • Earth rotation, • satellite orbits, • Earth gravity field
31 wikipedia.org
.. moves points due to • loading and • thermal deformation.
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Radial Deformation ur:
ps Surface pressure pref Reference pressure GR Green‘s functions
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10
mm
5
0
-5
-10
Atmospheric Loading
[Wijaya et al., 2011] Wettzell (non-tidal, IB)
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Conclusions
• Atmospheric corrections as determined from Numerical Weather Models play an important role in space geodesy, i.e., for the Earth gravity field, Earth rotation and figure of the Earth
• All parameters are available in real-time when determined from forecast data
• However, more research has to be carried out to reach the goals of GGOS: 1 mm in position and 0.1 mm/year in velocity
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THANKS FOR YOUR ATTENTION
We acknowledge the FWF for funding project ASPIRE (I1479) and ESA for funding project Tropsy.
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