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Subsections
In (1), we
introduce a new approach in which the
observed and forecast fields are broken down into a mixture of Gaussians and
the parameters of the Gaussian Mixture Model fit are examined
to identify translation, rotation and scaling errors.
We discuss the advantages of this method in
terms of the traditional filtering or object-based methods and
interpret resulting scores on a standard verification dataset.
[ read (pdf) online ].
In (2), we
introduce a set of
easily computable bulk statistics that
can be used to directly evaluate the performance of tracking algorithms
on specific characteristics.
We apply the evaluation method to a diverse set of radar reflectivity data
cases and note the characteristic behavior of five different storm
tracking algorithms proposed in the literature and now employed in widely
used nowcasting systems. Based on this objective evaluation, we devise
a storm tracking algorithm that performs consistently and better than any
of the previously suggested techniques.
[ read (pdf) online ].
In (3), we describe the AI competition that we (members of
the STAC commitee for AI in the American Meteo. Society) have been conducting
for the past two years and what we learned in each year.
[ read (pdf) online ].
In (4), we demonstrate that the availability of standards for the specification and transport of virtual globe data products has made it possible to generate spatially precise, geo-referenced images and to distribute these centrally-created products via a web server to a wide audience.
In this paper, we describe the data and methods for enabling severe weather threat analysis information inside a KML framework. The method of creating severe weather diagnosis products that are generated and translating them to KML and image files is described. We illustrate some of the practical applications of these data when they are integrated into a virtual globe display. The availability of standards for interoperable virtual globe clients has not completely alleviated the need for custom solutions. We conclude by pointing out several of the limitations of the general-purpose virtual globe clients currently available.
[ read (pdf) online ].
In (5), we describe offline analysis of Indian Doppler radar data from Cyclone Ogni using a suite of radar algorithms as implemented on NEXRAD and advanced algorithms developed jointly by the National Severe Storms Laboratory (NSSL) and the University of Oklahoma. We demonstrate the applicability of the various algorithms to Indian radar data, the improvement in the quality of the data and evaluate the benefit of nowcasting capabilities in Indian conditions using this data. New information about the tropical cyclone structure, as derived from application of the algorithms is also discussed in this study. Finally, we suggest improvements that could be made to the Indian data collection strategies, networking and realtime analysis. Since this is a first study of its kind to utilize doppler radar data in a tropical climate, the recommendations on realtime analysis and data collection strategies that we make, would in many cases, be beneficial to other countries embarking on Doppler radar network modernization programs.
[ read (pdf) online ].
In (6), we describe a technique that identifies candidate
bloom based on the range-variance of reflectivity in areas of bloom,
and uses the global, rather than local, characteristic of the echo
to discriminate between bloom and wide-spread rain. Every range gate
is assigned a probability that it corresponds to bloom using
morphological operations and a neural network is trained using this
probability as one of the input features. We demonstrate that this technique
is capable of identifying and removing echoes due to biological
targets and other types of artifacts while retaining echoes that
correspond to precipitation.
[ read (pdf) online ].
In (7),
a technique to identify storms and capture scalar features within the
geographic and temporal extent of the identified storms is described.
The identification technique relies on clustering grid points in an
observation field to find self-similar and spatially coherent
clusters that meet the traditional understanding
of what storms are. From these storms, geometric, spatial and temporal
features can be extracted. These scalar features can then be data mined
to answer many types of research questions in an objective, data-driven
manner. This is illustrated by using the technique to answer questions
of forecaster skill and lightning predictability.
[ read (pdf) online ].
In (8), an efficient sequential morphological technique
called the watershed transform is adapted and extended so that it can be used
for identifying storms. The parameters available
in the technique and the effect of these parameters are also explained.
The method is demonstrated
on different types of geospatial radar and satellite images.
Pointers are provided
on the effective choice of parameters
to target the resolutions, data quality constraints
and dynamic range found in observational datasets.
[ read (pdf) online ].
In (9), we extend our earlier study (published in IJCNN)
to use a set of 33 storm days and
demonstrate that it is possible to create a principled estimate of the probability of a tornado at a particular location within a circumscribed time window. The use of support vector machines for predicting the location and time of
tornadoes is presented.
We utilize
a least-squares methodology to estimate shear, quality control of radar
reflectivity, morphological image processing to estimate gradients, fuzzy
logic to generate compact measures of tornado possibility and support vector
machine classification to generate the final spatiotemporal probability field.
On the independent test set, this method achieves a Heidke Skill Score
(HSS) of 0.60 and a Critical Success Index (CSI) of 0.45.
[ read (pdf) online ].
In (10), we lay out the case for multi-radar, multi-sensor
weather applications, describe the WDSS-II framework and briefly
touch upon many of the WDSS-II applications including the display.
This is the paper to cite if you wish to cite WDSS-II from your
research papers.
[ read (pdf) online ].
In (11), we describe an automated technique to perform
quality control on WSR-88D reflectivity data.In this paper, we
use a neural network to combine the individual features, some of which
have already been proposed in the literature and some of which we
introduce in this paper, into a single
discriminator that can distinguish between ``good'' and ``bad''
echoes. The gate-by-gate discrimination provided by the neural network
is followed by more holistic post-processing based on spatial contiguity
constraints and object identification to yield quality-controlled
radar reflectivity scans that have most of the bad echo removed, while
leaving most of the good echo untouched.
The quality control algorithm described in this paper is compared
against the quality control algorithm currently used in operations
on the NEXRAD Radar Products Generator. A possible multi-sensor
extension to this technique is demonstrated.
Cite this paper to cite w2qcnn
[ read (pdf) online ].
In (12), A method for the detection of a bounded weak-echo region (BWER) within a storm structure that can help in the prediction of severe weather phenomena is presented. A fuzzy rule-based approach that takes care of the various uncertainties associated with a radar image containing a BWER has been adopted. The proposed technique automatically finds some interpretable (fuzzy) rules for classification of radar data related to BWER. The radar images are preprocessed to find subregions (or segments) that are suspected candidates for BWERs. Each such segment is classified into one of three possible cases: strong BWER, marginal BWER, or no BWER. In this regard, spatial properties of the data are being explored. The method has been tested on a large volume of data that are different from the training set, and the performance is found to be very satisfactory. It is also demonstrated that an interpretation of the linguistic rules extracted by the system described herein can provide important characteristics about the underlying process.
[ read (pdf) online at AMS website].
In (13), we describe a technique
for taking the base radar data, and derived products, from multiple
radars and combining them in real-time into a rapidly updating 3D merged grid
such that an estimate of that radar product combined from all
the different radars can extracted from these agents at any time.
We describe the model for the intelligent agents so as to account
for the varying radar beam geometry with range, vertical gaps
between radar scans, lack of time synchronization between radars,
varying beam resolutions between different types of radars, beam
blockage due to terrain, differing radar calibration and inaccurate
time stamps on radar data.
Further, we describe techniques for merging scalar products like
reflectivity as well as innovative, real-time techniques for combining
velocity and velocity-derived products. We also describe precomputation
techniques that can be utilized such that users can select a domain
and start seeing three-dimensional, combined radar data over that domain
in a matter of minutes. Finally, we also give pointers on derived
products that can be computed from these three-dimensional merger grids.
Cite this paper to cite w2merger
[ read (pdf) online ].
We develop a directional filter that is separable (14).
A directional filter allows you to smooth an image
without degrading edges.
A separable filter is computationally efficient, but
allows you to do logical operations on the pixels
(such as checking for missing data).
The separable filter is demonstrated on radar imagery.
[ read (pdf) online ].
Cite this paper to cite w2smooth
We describe a method (15) of multiscale storm identification,
computing motion estimates and making short range forecasts
from radar and satellite images.
[ read (pdf) online ].
Cite this paper to cite w2segmotionll/w2segmotioncg
In (16), I show how to speed up an elliptically-shaped filter so that
the filtering process can be carried out in real-time. The trade-offs that
this involves, including avoiding operations that are non-linear in the
initial stages are described.
[ read (html) online ].
This method can not deal with missing data. The fast method in (14) can.
In (17),
I describe how to set up a weather detection algorithm so that it is possible to tune that algorithm as more and more
cases get verified. I also discuss the possibility of being able to tune an algorithm to the local climatology. I demonstrate
this method on the BWER detection algorithm and describe the genetic algorithm that can make all this possible.
[ read (html) online ].
Gandin and Murphy showed that a measure they called the True Skill Score is unique in a property they call equitability.
In (18),
we show that it is impossible to come up with any measure that is
``equitable'' (infact, any measure that involves constraints of the form
posed by equitability) without making some rather daring assumptions.
The May issue of AI Applications carried this (19)
comprehensive paper on the fuzzy logic scheme to detect Bounded
Weak Echo Regions (BWERs) in radar images.
[ read (html) online ].
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V. Lakshmanan : valliappa.lakshmanan@noaa.gov