Purposes
and Programs of the
U.S. Weather Bureau National Severe Storms Laboratory
Norman, Oklahoma
Edwin
Kessler
Director, National Severe Storms Laboratory
1.
INTRODUCTION
The needs
for more accurate, timely, and meaningful weather information grow as
production, transportation, and communication processes become more intricate
and more weather-sensitive. Aviators, agriculturists, builders, shippers,
and insurers are among those who increasingly depend on information concerning
the present and forecast occurrences of storm hazards.
Development
of the national weather system to meet national needs efficiently depends
on the application of findings of basic and applied meteorological research.
Modern technology has produced numerous research tools whose coordinated-use
should contribute importantly to improved understanding of the meteorological
processes associated with severe storm development, to more accurate weather
analysis and forecasting, and to eventual beneficial modification or control
of weather including severe storms.
The National
Severe Storms Laboratory aims to extend our understanding of severe convective
phenomena such as tornadoes, hailstorms, and heavy rains. For the study
of these phenomena, modern weather radar is an indispensable tool, and
considerable specialization in techniques of radar data display and processing,
including synthesis of radar data with other kinds of information, is
required. It is natural, therefore, that the Laboratory also serve the
Weather Bureau as a research facility for development and applications
of radar to general meteorology and the national weather system.
2.
OBJECTIVES AND PROGRAM GUIDELINES
The Laboratory
objectives in the national interest are:
1. To gain
new knowledge of the morphology and dynamics of severe storms, such as
heavy rains, squall lines, thunderstorms and tornadoes, and thereby to
contribute to the development of improved forecasting, and understanding.
2. To discover
improved methods for collecting, analyzing, and processing severe storm
data, and to stimulate development of equipment, especially radar equipment,
holding promise of expanded capabilities.
3. To study
operating configurations of men and equipment, and thereby to contribute
to the design of improved storm observing and reporting systems wherein
sensors, processors and communications facilities are efficiently meshed
to provide timely, accurate information to the host of users.
The National
Severe Storms Laboratory has objectives of investigation formerly addressed
by the National Severe Storms Project at Kansas City, Mo. and by the Weather
Radar Laboratory at Norman, Okla., and will emphasize the applications
of radar and aircraft probes, and surface networks of closely spaced automatic
recording stations for these studies. A great variety of severe weather
occurs near Norman, and the co-located University of Oklahoma and its
Atmospheric Research Laboratory will furnish important and unique support
to the Laboratory mission (figure 1).
Figure 1. Aerial
view showing University of Oklahoma Research Park, Norman, Oklahoma,
with buildings housing the USWB's National. Severe Storms Laboratory,
and other facilities.
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The shape
of the NSSL program at a particular time will naturally be determined
by the interests and capabilities of participating personnel. The national
problem of skilled manpower shortage will certainly be reflected in the
scope of the program. A few highly qualified specialists will be retained
as consultants, and every reasonable effort will be made to attract capable
people with interests in all the physical and mathematical disciplines
needed to advance meteorological frontiers.
The decision
to work on a particular task will be based on considerations of the importance
of the problem, the reasonableness of the proposed approach to a solution,
and the adequacy of available resources to secure a desired useful result.
Financial
resources, equipment, and facilities authorized for NSSL management will
be allocated to in-house or contractor control on a basis of estimated
benefits per unit expenditure. Many intangibles enter such estimates.
Government, university, and commercial enterprises have distinctive characteristics
which may determine the type of facility best suited to particular tasks.
3.
ORGANIZATION
Organization
of the National Severe Storms Laboratory is outlined in figure 2. The
Laboratory is responsible to the Office of Meteorological Research, and
will receive guidance from consultants drawn from institutions of government,
commerce, and education. The interests of other agencies will be made
known through the office of the Chief, U.S. Weather Bureau, and by contacts
at other levels.
The activities
of research and equipment development shown in figure 2 are the Laboratory's
raison d'etre. All other activities are supporting and their value
will be judged in terms of their support effectiveness.
Not all
of the activities suggested by figure 2 will be fully staffed by
NSSL employees. Some activities may be staffed by contractors or by the
employees of other government agencies. Some work may be funded by transfer
of monies to NSSL management from other agencies.
Figure 2. General
organization of NSSL, Norman, Oklahoma. In practice, it is common
for single individuals to participate in different activities
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4.
PROGRAMS
During past
seasons, weather reconnaissance and weather penetration aircraft of cooperating
agencies and of the U.S. Weather Bureau have been used with observations
of radar and a network of closely-spaced surface observation stations,
and with synoptic data, to describe atmospheric states and physical processes
associated with thunderstorms and related weather systems. Findings and
conclusions have been documented in the reports of the National Severe
Storms Project [1-19 and others, in press]; these are important to the
planning of future work.
The coordinated
use of modern observing equipment will continue to be emphasized at NSSL;
important and difficult tasks will be the design of experiments
to take greatest possible advantage of complementary observational capabilities.
Of course,
it is not possible at the outset to map the forthcoming program in detail.
Foci of effort will be determined by need and the availability of good
ideas and sufficient resources. Some problem areas which may receive active
attention at NSSL are discussed briefly in the following sections:
A. Measurement
of precipitation rate by radar - This task requires correlation
between radar and rain gage observations and will utilize digital computers
for radar data processing (see fig.3) and assembly of rain gage data from
stations maintained by the Laboratory* and the Agricultural Research Service,
Chickasha, Okla. ** Austin [20], Wilson [21] and others have demonstrated
the potential accuracy of the WSR-57 for rainfall measurements in widespread
precipitation. Their works must be extended to include many cases of highly
variable precipitation. It is expected that radar can provide information
of rainfall occurrences so timely and accurate that flash-flood forecasting
will be greatly improved, with resultant saving of lives and property
and more economical utilization of reservoirs and hydroelectric facilities.
The tasks of applying precipitation rate-radar echo relationships to problems
of stream flow and ground water are within the jurisdiction of the Office
of Hydrology, U.S. Weather Bureau; the Corps of Engineers, U.S. Army;
and the Department of Agriculture.
Accurate
measurement of precipitation rate on a small scale should also contribute
to establishment of criteria for severe storm identification and to analysis
of the water and energy
budget of storms: knowledge of budget parameters is essential to the understanding
of storm mechanics.
Figure 3. Digitized
distribution of radar echo intensities within 100 nm. of Norman,
Okla., August 7, 1963, as produced by a computer from series of
WSR-57 radar observations. A photograph of the plan position indicator
with high radar sensitivity is also shown.
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B. Application
to air traffic control of ground-based weather radar and sferics equipment
- Incidents associated with flights of aircraft in the vicinity of
thunderstorms have emphasized the need for more knowledge of associations
between thunderstorm echoes and turbulence and improved application of
observing tools to problems of air safety. With the aid of ground-based
radars, high-performance aircraft will be vectored through and near thunderstorm
areas while sferics counts and distributions of radar reflectivity are
simultaneously recorded.*** These data should reveal the frequency distributions
of significant parameters of atmospheric turbulence, electricity, and
hail which are characteristic of particular altitudes, and of radar and
sferics indications. Findings should provide a basis for rational estimation
of the economic and human factors associated with flight through particular
weather conditions and, thus, for operational decisions which incorporate
these factors.
C. Doppler
radar - Doppler radar [22] can measure the radial speeds of scattering
elements, hence can be a basis for deducing much information about winds
[23], and probably holds the greatest potential of all the new tools for
expanding man's knowledge of wind fields accompanying precipitating weather
systems. Doppler data can be used to infer distributions of precipitation
particle size, and contribute to understanding of the microphysical processes
fundamental to precipitation production [24, 25]. Recent applications
of Doppler have contributed to better understanding of the nature of radar
echoes from invisible sources, the radar "angels," and suggest advanced
techniques which may provide a needed breakthrough in the study of clear-air
turbulence [25, 26].
The width
of the Doppler spectrum from precipitation depends on the variation of
radial speeds among the scattering particles and may be a measure of aircraft-sensed
turbulence; an R-meter [27] attachment permits a conventional radar to
estimate spectrum width also [28]. NSSL will use aircraft with Doppler
and conventional radars to search for a suitable means for identifying
locations of severe turbulence quickly and economically. Research success
would be quickly translated into benefits for aviation meteorology.
The application
of Doppler techniques to meteorology is rather new and special signal-processing
techniques are necessary; at present there are very few, Doppler weather
facilities. Because of the great potential of Doppler radar, NSSL is developing
an installation for use by its staff and other meteorologists (fig. 4
and [29]).
Figure 4. Mobile
X-Band pulsed Doppler radar at NSSL. At present, peak power is 6
kw. and the pulse repetition frequency is variable to 10 kc./sec.
half-power beamwidth is 1.39
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D. Wind
and water distributions and energy conversion and transport processes
- Our capabilities for forecasting and controlling severe storms will
be advanced by knowledge of associated air circulations and energy transformation
processes; this requires that observations observation must be used, because
significant storm details are distributed on small space and time scales.
Aircraft should provide photographs, from which the shape of clouds can
be accurately mapped, and measurements of temperature, pressure, wind,
and water content (fig. 5); radar reflectivity data can be a basis for
estimates of 3-dimensional distributions of precipitation content; the
observations of surface stations separated by mesoscale lengths provides
rainfall and wind data essential to water budget considerations, and the
surface distributions of pressure and temperature. These considerations
have been discussed in detail by Braham [30], Atlas [31], and Fujita [32],
for example.
At NSSL,
a great part of the program will be devoted to developing improved syntheses
of severe storm observations and theories. In this regard, the ideas of
Lhermitte [23], Browning [33], Kessler [34], and 0gura [35] suggest important
possibilities.
Figure 5. The
importance of aircraft observations is illustrated by this cross-section
of the water vapor distribution across a dry line in northwestern
Oklahoma. The locations of observations made along the aircraft
flight path are indicated by dots. The vertical orientation of the
zone of abrupt moisture change, its extremely narrow horizontal
extent, and details of the moisture distribution in the humid air
could not be delineated except from aircraft measurements.
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E. Statistical
characterization of weather patterns, and implications - The development
of applications for radar-derived and satellite-derived information has
been slowed in
part by difficulties of objective pattern description. The availability
of large high speed
digital computers now permits advances in this important area [35, 36,
37, 38]. For
example, objective measures of pattern bandedness and orientation, the
characteristic length of pattern elements, and pattern motion and development
can all be determined
with computer-performed correlation routines. The average radar-echo intensity,
the intensity variance, and the proportional area covered by echoes have
been shown
to discriminate among radar echo patterns. Since pattern parameters are
correlated with
each other! not all are essential to a comprehensive description of pattern
statistics. The
description of a weather pattern by a minimum number of variables is important
to the economical
communication of weather intelligence.
The relationship
of radar echo and satellite photograph pattern parameters to severe storm
occurrences and to synoptic weather features is important to the coordinated
use of the conventional observing tools with the new. Studies like [38]
which relate the predictability of scale weather patterns to other pattern
descriptors should be extended. Techniques such as multiple discriminant
analysis [39] should be used in this work.
Other important
problems concern relationships among statistical properties of storm patterns
and the associated turbulence, momentum and energy transport and conversion
processes, and the large scale flow.
F. Meteorological
systems analysis and advanced instrumentation - Studies
of various configurations of men and equipment are necessary to incorporate
new techniques for observing and reporting storms into effective operational
routines. System studies may be undertaken at the request of the Systems
Development Office and other sponsoring organizations and in partnership
with responsible groups; in some cases, Laboratory personnel may have
consulting roles. Reports of such studies will include recommendations
concerning needs for specialized equipment ([41- 42, 43, 44], for example)
for operational data collecting, processing, and communicating.
In the research
programs, much data may be usefully reduced by hand and processed in established
facilities, but development and procurement of some specialized equipment
will probably also be necessary. The effective combination for research
purposes of data from aircraft/ radar and mesonetwork sources, and the
speedy, comprehensive analysis and recording of Doppler radar spectra,
for example, may depend on equipment development or procurement by the
Laboratory.
5.
PUBLICATION OF RESULTS
Important
results of NSSL investigations will be offered as soon as possible after
their completion for publication in scientific journals. The prepublication
series represented by this report will be used for disseminating information
more rapidly and in more detail than is practicable via formal publication.
*In spring
1964, a 47-station network for comprehensive mesoscale weather observations;
see Appendix.
** In spring
1964, 173 recording rain gages over 1128 sq.mi. for rainfall-runoff studies
along the Washita River and tributaries; see Appendix.
***Of course,
even high-performance aircraft must be guided to avoid areas where the
a priori probability of extremely severe weather is judged to be
high.
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