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New developments and operational experience with
surface observation technology and national
networks
Jitze P. van der Meulen,Royal Netherlands Meteorological
Institute
TECO 2006
2006-12-04 TECO-2006 2
Historic Background 1643: Evangelista Torricelli discovers
vacuum invents mercury barometer and suggested p
1645:René Descartes suggests p = p(h)
1650: Blaise Pascal and Robert Boyle, by experiment: p & p = p(h), using a mercury barometer
All using calculus: hydrostatics & mathematics
2006-12-04 TECO-2006 3
Historic Background 1802: Alexander von Humboldt,
explorer to discover environmental phenomena: t = t(h), later on with Joseph-Louis Gay-Lussac
< 1850: phenomenological studies with a deterministic approach, e.g. networks to measuring the intensity of Earth's magnetic field
> 1850: use of mathematics comes up and experiments produce quantitative data to prove any theory by calculus
Discovery of phenomena (qualitative), later on mathematics (quantitative)
2006-12-04 TECO-2006 4
Historic Background > 1835: networks to measure the
geological behavior of the earth electromagnetic field in combination with barometers and themometers, to discover any correlation
Measurements of the variable behaviour of atmospheric pressure: a relation with wind (speed and direction) was discovered
Tendency of pressure useful to forecast weather (still popular today at home )
Geospatial relationship of pressure gradients and the behaviour of wind
Discovery of phenomena
2006-12-04 TECO-2006 5
Historic Background > 1845: introduction of Telegraphy,
providing in "near real time“ and synoptic surface observations to be plotted in synoptic charts (a ‘nearly instantaneous picture of the state of the atmosphere’)
1900: postulation that hydrostatic formulas could be used to describe the current state of the atmosphere and for forecasts (‘calculating the weather’)
> 1945 introduction of operational upper air measurements and NWP
Use of geophysical data in weather charts, calculus requires “infinite amount” of arithmetics
2006-12-04 TECO-2006 6
Historic Background
2006-12-04 TECO-2006 7
Historic Background Today: Both science and operational services
(meteorology, climatology, etc.) are oriented on both
– discovery of weather phenomena(the classic deterministic approach), and on
– thermodynamics with plenty of mathematics (used in NWP & NCP models).
This statement not only holds for in situ measurements but also for remote sensing and especially for observations from satellites (Earth Observation).
2006-12-04 TECO-2006 8
Systems development and functional requirements functional specifications of networks and weather
stations have a complex background A network should provide
– present weather information expressed in pre-defined parameters, like type-of-cloud, special phenomena, type-of-precipitation, icing
– numerical data, i.e. quantitative physical variables
Complex? Simple compared to the present needs of the multiform disciplines in meteorology and the available technologies of observation, both in situ and remotely sensed
2006-12-04 TECO-2006 9
Systems development and functional requirements Development of observing systems, in
particular those systems based on satellite born remote sensing ('discovery' entity, but also producing quantities)
Geospatial differences in network densities Differences in representativety (area averaged
vs. point measurements) Differences in observation times and
frequencyin situ satellite
2006-12-04 TECO-2006 10
Systems development and functional requirements Development of observing systems, in
particular those systems based on satellite born remote sensing ('discovery' entity, but also producing quantities)
Geospatial differences in network densities Representativety (area averaged vs. point
measurements)
wind derived from the ERS-2 scatterometer, south- east of Greenland, 2006-10-15 21:30 UTC
2006-12-04 TECO-2006 11
Systems development and functional requirements The various disciplines in meteorology,
climatology, hydrology, etc. expressed an increasing demand on observational data and with discipline specific conditions.
Alternative or new observations, performance, representativety and frequency of observations.
Complete automation (of subjective observations, present weather, phenomena), modern AWS
Strong increasing diversity in both the users' requirements and in observation technology
2006-12-04 TECO-2006 12
Systems development and functional requirements
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OBSERVATIONS
[Sy] Synoptical Meteorology, [Cl] Climatology, [Hy] Hydrology, [Ag] Agro-meteorology, [Ae] Aeronautical meteorology, [Ma] Marine meteorology, [AS] Sciences of the atmosphere .
2006-12-04 TECO-2006 13
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database oriented information generators
Systems development and functional requirements
2006-12-04 TECO-2006 14
Systems development and functional requirements Defining functional specifications of physical variables to
be measured is relatively straightforward: measurement uncertainty can be expressed quantitatively and references are clearly defined.
To specify quality figures for reporting weather events, atmospheric conditions or qualitative descriptions (the assessment of the state and development of the atmosphere, and of significant weather) is complicated and affected by subjectivity:E.g., shall we use performance indicators like
Skill scores Success rates False alarms rate, or A mixture of these?
2006-12-04 TECO-2006 15
Systems development and functional requirements A contingency matrix is most applicable, but
how to interpret?
detector
yes no
reality yes a b
no c dProbability of Detection: a / (a + b)False Alarm Ratio: c / (a + c)Equitable Skill Score: a / (a + b) – c / (c + d)BIAS = (a + b) / (a + c) [should be 1]
Event?
2006-12-04 TECO-2006 16
Performance indicators
detector
yes no
realityyes 15% 5%
no 5% 80%
POD = 75%FAR = 25%ESS = 69%BIAS = 1
‘overall score’ ?
range ?: e.g. ‘icing’ most relevant: ‑2°C < T < +2°C
2006-12-04 TECO-2006 17
Systems development and functional requirements New challenge: observations in
combination with a high resolution model: using the actual NWP grid-point data as
background (e.g. 11 km grid) Using a detailed orographic database
(relief map) Climate data for further fine-tuning +
knowledge of atmospheric behavior in land-water transitions
Now-casting technique with ‘downscaling’ capabilities
50 km
Virtual reality ?
2006-12-04 TECO-2006 18
Systems development and functional requirementsMethods of observing Present
Weather, also virtual reality? Determination based on empirical
relations Direct and indirect phenomenological
en physical relationships are applied Climate data as filter tool Algorithms, tuned for optimal
performance
2006-12-04 TECO-2006 19
Systems development and functional requirements
Methods of observing Present Weather, also virtual reality?
Examples: Undercooled precipitation using wet &
dry bulb temperature Hail detection from doppler weather
radars Precipitation determination based on
optical characteristics of the hydrometeors in combination with air temperature
2006-12-04 TECO-2006 20
Systems development and functional requirements
Methods of observing Present Weather, also virtual reality?
Data from the true world is not available, so validation is a hazardous task
How to calibrate? What is a reliable reference?
Algorithms are not well documented and published
A quality standard for such determination is missing (may be in line with ISO 17025)
2006-12-04 TECO-2006 21
Development and new design of instruments Clustering of sensors/instruments, e.g. on
one single statue discarding the mutual impacts
2006-12-04 TECO-2006 22
Development and new design of instruments Clustering of sensors/instruments, e.g. on
one single statue discarding the mutual impacts
Micro-sized systems with 'multi-sensors on a single chip'
wind sensor
2006-12-04 TECO-2006 23
Development and new design of instruments Clustering of sensors/instruments, e.g. on
one single statue discarding the mutual impacts
Micro-sized systems with 'multi-sensors on a single chip'
Pressure sensor
2006-12-04 TECO-2006 24
Development and new design of instruments Clustering of sensors/instruments, e.g. on
one single statue discarding the mutual impacts
Micro-sized systems with 'multi-sensors on a single chip'
Introduction of ‘alternative’ techniques
holograms
monostatic radar: drop size distribution
‘Hotplate snowgauge’ Acoustic detector
2006-12-04 TECO-2006 25
Trends and criteria for further development, a conclusion Ongoing development of new methods of
observation and measurement devices Satellite born remote sensing techniques to
observe the surface of the whole earth Ongoing automation of weather stations,
automation of observing the weather All kind of observations to be converted into
geo-physical quantities Determination of weather parameters based
on phenomenological assumptions
2006-12-04 TECO-2006 26
Trends and criteria for further development, a conclusion Priority on efficiency and cost reduction Observation systems and networks will be
further optimized; wish to integrate observing systems; surface variables determined from in situ (surface) and remote sensing (satellites) data
Automation of subjective observations to be standardized or at least well documented in open literature; requirements on skill scores
Focus on specific, dangerous weather events, and on methods of observations to improve the performance of NWP
2006-12-04 TECO-2006 27
Thank you