Institute of Meteorology and Water Management New Meteorological Satellites – selected applications for agrometeorology PIOTR STRUZIK IMWM Kraków.

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Transcript Institute of Meteorology and Water Management New Meteorological Satellites – selected applications for agrometeorology PIOTR STRUZIK IMWM Kraków.

Institute of Meteorology and Water Management
New Meteorological Satellites
– selected applications for
agrometeorology
PIOTR STRUZIK
IMWM Kraków
Presentation outline:
1. Meteorological satellite system – actual status and near
future in Europe.
2. MSG and EPS satellite systems and their applications in
agriculture:
- surface temperature,
- soil moisture,
- vegetation (including forest fires),
- solar radiation.
3. Future satellite missions.
4. Conclusions.
MSG in EUMETSAT’s overall
Satellite Systems
96
METEOSAT
97
98
99
00
01 02
Operational S/C (until June 1998)
Meteosat-7
MSG
MSG-1
MSG-2
MSG-3
MSG-4 (TBC)
EPS
METOP-1
METOP-2
METOP-3
04
05
06
07
Hot stand by (at 10° East, until 14/1/98) IODC (63° East)
Meteosat-5
Meteosat-6
03
08 09
10
11
Operational
Approved
Fuel margin
Available
12
MSG
EUMETSAT
Applications
Ground
Segment
EPS/Metop
Data acquisition
and control
Pre-processing
EUMETSAT HQ
Direct
read-out
service
HRPT
Applications Ground Segment
Products extraction
EUMETSAT HQ
Centralised
processing
and generation
of products
Unified Meteorological
Archive and Retrieval
Facility (U-MARF)
EUMETSAT HQ
USERS
SATELLITE
APPLICATION
FACILITIES
Decentralised
processing
and generation
of products
MSG Solutions
 Temporal resolution: 15 minutes instead of 30
minutes
 Spatial sampling at sub-satellite point:
3 km (1 km HR VIS) instead of 5 km (2.5 km VIS)
 More channels:
1 HR VIS, 2 VIS, 1 near IR, 4 IR windows, 2 WV, 1
Ozone and 1 CO2
 Exploitation of data separated into general
processing centrally by EUMETSAT and specialised
processing by specific centres (SAF)
MSG 1 km Resolution
MSG 3 km Resolution
Meteosat IR Resolution
Meteosat IR Channel ~ 5 km
Meteosat VIS Channel ~ 2.5 km
IMPROVED SPATIAL
SAMPLING WITH THE
HRV CHANNEL
(Example: 4 December 2002,
12:30 UTC)
MSG HRV channel ~ 1 km
EUMETSAT SAF activities related to
agrometeorology:
• NWC SAF
• Land SAF
• Climatological SAF
• Hydrological SAF (in creation process)
Types of activities:
•Operational products
•Software packages
SW Packages for Users
SEVIRI

Cloud Mask

Cloud Type

Cloud Top Temp. & Height

Precipitating Clouds

Convective Rainfall Rate

Total Precipitable Water

Layer Precipitable Water

Stability Analysis Imagery

High Resolution Winds

Aut. Sat. Image Interpr.

Rapid Dev.
Thunderstorms

Air Mass Analysis

Improved Obs. Operators
(for AMVs)

Geostationary Rad.
Assimilation
AAPP
AVHRR/AMSU/MHS/HIRS

Improved and extended

Cloud Mask
versions for annual

Cloud Type
distribution (e.g. updated

Cloud Top Temp. & Height
ingest function, updated

Precipitating Clouds
cloud detection, added ICI

Improved & Extended RTMs
retrieval module etc.)
IASI

Fast RTM & Obs. Operators  Extension to processing
IASI+AMSU+AVHRR
GOME

Obs. Operators
ASCAT/SeaWinds

Improved Obs. Operators
SSM/I

1DVar Retrieval System
SAF NWC
(for wind speed, cloud water
SAF NWP
etc.)

Fast RTM
SSMIS

1DVar Retrieval System
(for wind speed, cloud water
etc.)

Fast RTM
AIRS

1DVAR Retrieval System
Real Time Product Services related to agrometeorology
MSG








Surface Albedo
Scattered Radiance Field
Surface Short-wave
Fluxes
Land Surface
Temperature
Surface Emissivity
Surface Long-wave
Fluxes
Soil Moisture
Evapotranspiration Rate
EPS









Near Surface Wind
Vector
Surface Albedo &
Aerosol
Scattered Rad. Field
Surface Short-wave
Fluxes
Land Surface
Temperature
Surface Emissivity
Surface Long-wave
Fluxes
Evapotranspiration Rate
N. Europe Snow Cover
Multi-Mission




Land Surface Temperature
Surface Emissivity
Surface Long-wave Fluxes
S. & C. Europe Snow
Cover
SAF
SAF
SAF
SAF
SAF
OSI
O3M
CLM
GRM
LSA
MSG






Surface Albedo & Aerosol
Scattered Radiance Field
Surface Short-wave
Fluxes
Land Surface
Temperature
Surface Emissivity
Surface Long-wave
Fluxes
SAF
SAF
SAF
SAF
SAF
OSI
O3M
CLM
GRM
LSA
Off-Line Product Services
EPS






Surface Albedo & Aerosol
Scattered Radiance Field
Surface Short-wave Fluxes
Land Surface Temperature
Surface Emissivity
Surface Long-wave Fluxes
Multi-Mission







Land Surface
Temperature
Surface Emissivity
Surface Long-wave
Fluxes
NDVI, FGV, fPAR, LAI
Surface Rad. Budget
Surface Albedo
Rad. Budget at TOA
Real Time Product Services
EPS









Surface Albedo (1 km, 12 hours)
Aerosol (1 km 12 hours)
Scattered Radiance Field (1 km, 12 hours)
Surface Short-wave Fluxes (1 km 12 hours)
Land Surface Temperature (1 km, 6 hours)
Surface Emissivity (1 km, 6 hours)
Surface Long-wave Fluxes (1 km, 6 hours)
Evapotranspiration Rate (1 km, TBD)
N. Europe Snow Cover (1 km, 1 day)
OSI
O3M
CLM
GRM
LSA
Off-Line Product Services
EPS







Surface Albedo (1 km, 10 days & 1 month)
Aerosol (1 km, 10 days & 1 month)
Scattered Radiance Field (1 km, 10 days & 1 month)
Surface Short-wave Fluxes (1 km, 10 days & 1 month)
Land Surface Temperature (1 km, 10 days)
Surface Emissivity (1 km, 10 days)
Surface Long-wave Fluxes (1 km, 10 days)
OSI
O3M
CLM
GRM
LSA
Potential data delivery from H-SAF during the operational phase (2010-2014)
Resolution (Europe)
Accuracy
Cycle (Europe)
Timeliness
10 km (with CMIS)
15 km (with other
GPM)
10-20 % (rate > 10 mm/h), 20-40 % (rate 1 to 10 mm/h), 40-80 % (rate
< 1 mm/h)
6 h (with CMIS only) 3 h (with
full GPM)
15 min
Precipitation rate merging MW
& IR
10 km
Ranging from MW performance to degraded one to an amount to be
assessed
15 min
5 min
Water phase (based on MW)
10 km (with CMIS)
15 km (with other
GPM)
80 % probability of correct classification
6 h (with CMIS only) 3 h (with
full GPM)
15 min
3, 6, 12 and 24 h cumulated
rain
10 km
Depending on integration interval. Tentative: 10 % over 24 h, 30 % over
3h
3 hour
15 min
Product
Precipitation rate from MW
imagery
(from merged MW +
IR)
Soil moisture in the surface
layer
25 km (from ASCAT)
CMIS)
40 km (from
0.05 m3 m-3 (depending on vegetation)
36 h (from ASCAT) 6 h (from
CMIS)
2h
Soil moisture in the roots
region
25 km (from ASCAT)
CMIS)
40 km (from
To be assessed (model-dependent). Tentative: 0.05 m3 m-3
36 h (from ASCAT) 6 h (from
CMIS)
2h
Snow recognition
5 km (in MW)
2 km (in
VIS/SWIR/TIR)
95 % probability of correct classification
6h
2h
Snow effective coverage
10 km (in MW)
5 km (in
VIS/SWIR/TIR)
15 % (depending on basin size and complexity)
6h
2h
80 % probability of correct classification
3 h (under cloud-
Snow thawing-freezing
conditions
5 km (in MW)
2 km (in TIR)
Snow status (wet or dry)
5 km
80 % probability of correct classification
6h
2h
Snow water equivalent
10 km
To be assessed. Tentative: 20 mm
6h
2h
Selected satellite products and their applications
Potential users market
Agriculture
Forestry
Natural hazard management
Terrestrial transports safety
Land SAF products
User extra effort
Land Surface Temperature
High
Soil Moisture
Low
Evapotranspiration
Low
Biophysical Parameters
Low to middle
Albedo
Low
Land Surface Temperature
Low to high
Evapotranspiration
Low
Biophysical Parameters
Low
Albedo
Low
Land Surface Temperature
Low to High
Soil Moisture
Low
Evapotranspiration
Low
Snow Cover
Low
Biophysical Parameters
Low
Land Surface Temperature
High
Snow Cover
High
Data Sources for Soil Moisture
Measurements
• Field Observations
– Expansive
– Only a few measurement networks (agrometeorologic)
• Remote Sensing most promissing
– Global & Frequent
– Cost efficient
• Microwave Remote Sensing most suitable
– Offer the most direct means due to sensitivity to the dielectric
properties
– Day and night capabilities
– Independent of Clouds
– Problem: vegetation, surface roughness
Soil moisture vs. thermal inertia – problems with cloud cover !
Available Microwave Sensors
• Passive Sensors (Radiometers)
– SSMR (1978 - 87)
– AMSR (2002 - )
– CMIS (2009 - )
– SMOS (2007 - )
– HYDROS (2010 - )
• Active Sensors (Scatterometers)
– ERS Scatterometer (1991 - )
– METOP ASCAT (2005 - )
– HYDROS (2010 - )
From ERS to METOP
•
ERS Scatterometer
– 1991 up to present
– 3 antennas
– 50 km spatial resolution
– Daily coverage < 41 %
•
METOP Advanced Scatterometer
– start in 2005
– 6 antennas
– 25 km resolution
– Daily coverage > 80%
Source: Klaus Scipial 2004
Surface temperature on the area of Poland
Drought in Poland - 1993
2nd half of July
2nd half of August
Vegetation indices
3rd decade of September
Fires/Smoke
Channel 04 (3.9 m)
Channel 07 (8.7 m)
Fires over Portugal and Spain (biggest fires of last 20 years)
MSG-1, 3 August 2003, 12:00 UTC
Institute of Meteorology and Water Management
POLAND
The World Radiometric Network (1964-1993)
W/m2
800,00
700,00
600,00
18.10.99
19.10.99
500,00
20.10.99
400,00
21.10.99
22.10.99
300,00
25.10.99
200,00
26.10.99
27.10.99
100,00
28.10.99
0,00
430
29.10.99
530
630
730
830
930
1030
1130
1230
1330
1430
1530
Tim e
Daily variation of Solar radiation regitered at the ground by
pyranometer 18-30.10.1999 Krakow.
30.10.99
Pyranometr
Satelita
10000
6000
4000
2000
XI
XII
I
IV
V
VI
VII
VIII
Daily available solar energy on XI.1999 - IX.2000 registered by
pyranometer and estimated from satellite data (location Krakow,
Poland).
IX
30
22
14
6
30
22
6
14
30
22
14
6
29
21
13
5
29
21
13
5
28
20
12
4
28
20
4
III
12
26
18
2
II
10
26
18
10
2
26
18
10
2
25
9
17
0
1.XI
Wh/m2
8000
8000
7000
Satellite [Wh/m2]
6000
5000
4000
3000
2000
1000
0
0
1000 2000 3000 4000 5000 6000 7000 8000
Pyranometer [Wh/m2]
Comparison of daily solar energy registered at the ground at estimated from satellite data
(period XI.1999 - IX.2000, Kraków).
Severe
weather
warnings
Combined
satellite and
lightning
detection data
Future satellite missions interesting for
agrometeorological applications
• SMOS (Soil Moisture and Ocean Salinity Mission) 2007,
• GPM (Global Precipitation Mission) planned 2008,
postponed to 2010 – 2015,
• Active radar satelites with resolution 8 m – 2006
(Germany),
Conclusions:
1. Operational applications of MSG satellite are becoming
available.
2. EPS products are expected in 2006.
3. Main use of MSG satellite products is as an input to
agrometeorological models (irrigation, pest & disase
etc.). Also use for severe weather warnings.
4. We are still far from direct operational use of satellite
products in agrometeorology (models required).
Sensing does not tell us why fire is
hot, just that it is hot.
(Aristotele, Metaphysicorum liber)