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Latest News: Mar 29
2008: JRA25, NCEP and NCEP2 are updated
to Feb 2008. |
Introduction
This is the Home page for the
We present the global statistics of cyclones
that were tracked with the
The primary purpose of this web site is to
allow the wider community to access our cyclone statistics, which are available
on a 2.5 x 2.5 degree latitude-longitude grid, and to
perform a variety of tasks including the creation of plots, the saving of data
and the computation of anomalies (difference) from a chosen reference data set
e.g. a climatology.
Cyclone statistics based on 6 hourly mean
sea level pressure (MSLP) are available for several reanalysis projects: ERA-40 Reanalysis (ERA40)
(1957-2002), NCEP
Reanalysis (NCEP) (1958- ongoing), NCEP Reanalysis 2
(NCEP2) (1979- ongoing) and JRA-25 Reanalysis
(JRA25) (1979- ongoing).
A long term goal is to allow the
user to access the tracks database from which the statistics are derived.
Details about our group are
available here:
Meteorology Group,
Cyclone
statistics
This version (1.0) supersedes
the beta version that has been operating since May 2006. See the Help section for
documentation. This mainly consists of Basic
Help
and an Example. The web site is
designed to be fairly self-explanatory.
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You may
access the cyclone statistics web site at: http://www.earthsci.unimelb.edu.au/tracks/cycstats/cycstats.php |
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Please Note: Our network is backed up nightly from
18:00-24:00 (UTC +10:00) and so there may be poor response at times during
this period. Furthermore, the temporary directories created for a user are
deleted at 17:10 each Tuesday, Thursday and Sunday. |
Please direct any
questions or report any problems to Kevin
Keay.
The
The cyclone tracking software is freely
available from our group. It is written in Fortran 77 and should compile
correctly on any platform with the GNU g77 compiler. To date it has been
compiled successfully on systems running Solaris, Linux and Cygwin
under Microsoft Windows 2000 (and presumably under Windows XP). The present
version is designed for grids of the order of 1 degree or larger, including the
widely-used 2.5 degree reanalysis pressure and geopotential
height fields. There is also a new version that can accommodate grids between
0.25 and 1 degree. This has not been exhaustively tested by us but we have
assisted a small number of users with data on a 0.25 degree grid and the
results appear fine. The input data should be in a simple binary format that we
refer to as conmap. Details of this format are
given in the software documentation. We can provide some additional Fortran 77
software to assist in converting GRIB or NetCDF data
to the conmap (CMP | CIF) format. At present there is
no graphics capability for external users but we are looking into providing
scripts for a freely available package such as GrADS.
The software may be obtained by contacting Ian Simmonds.
Please indicate the platform that you
intend to run the software on. We recommend the g77 compiler but the software should compile with others but we cant
test these ourselves. In addition please tell us the resolution of the data
that will be input to the software. Often a user will contact us again if they
require any further assistance on matters such as choice of parameters or to
convert NetCDF to conmap if
no appropriate tools are available.
The animation at the top of this page
The animation at the upper right of this
page shows cyclones that were identified on six-hourly mean sea level maps from
the ERA-40 Reanalysis which is freely available from the ECMWF. See: http://data.ecmwf.int/data/d/era40_daily
The period July 1 2001 00UTC July 4 2001
18UTC (16 maps) is shown. Different symbols depict the cyclone state as shown
in this key:

The term strong is relative. In this
example it refers to cyclones with a mean Laplacian of pressure exceeding 0.2 hPa/(deg.lat.)2
but often one would choose a larger value e.g. 0.7, to highlight the stronger
systems. Click here for a larger animation (1.1 MB).
Sources of Data
The cyclone statistics presented here are
based on 6 hourly mean sea level pressure (MSLP) fields from several reanalysis
projects. These are freely available from the following web sites (note that
registration is required for access to JRA25 products):
1.
ERA-40
Reanalysis (ERA40) (1957-2002)
2.
NCEP Reanalysis
(NCEP) (our statistics: 1958- ongoing)
3.
NCEP Reanalysis 2
(NCEP2) (1979- ongoing)
4.
JRA-25 Reanalysis (JRA25) (1979- ongoing)
Copyright and Disclaimer
We use the cyclone statistics that are
presented here in our published research. Although every effort has been made
to ensure that they are correct we can not guarantee that the statistics or the
data used to compute them are free from errors. Hence we take no responsibility
for any negative consequences arising from their use by any party external to
our group at the
The cyclone statistics, as data files or
images, may be freely used for research and most
publications including journals. However in the case of a reference book (e.g. an encyclopaedia) or
a text book you should contact Ian Simmonds for clarification on any
potential copyright issue relating to the
In any event it would be appreciated that
you include an appropriate reference to this web site. For instance:
The cyclone statistics
were obtained from the
Murray, R. J., and I. Simmonds, 1991a: A numerical
scheme for tracking cyclone centres from digital
data. Part I: Development and operation of the scheme. Australian
Meteorological Magazine, 39, 155166.
Murray, R. J., and I. Simmonds, 1991b: A
numerical scheme for tracking cyclone centres from
digital data. Part II: Application to January and July general circulation
model simulations. Australian Meteorological Magazine, 39, 167180.
Simmonds,
Simmonds,
Simmonds,
Lim, E.-P., and I.
Simmonds, 2007: Southern Hemisphere winter extratropical cyclone
characteristics and vertical organization observed with the ERA-40 reanalysis
data in 1979-2001. Journal of Climate, 20, 2675-2690.
References
Rice, J., 1982: The Derivation of a Computer-based
Synoptic Climatology of Southern Hemisphere Extratropical Cyclones. Honours Thesis, Department of Meteorology, The
Murray, R. J., and I. Simmonds, 1991: A
numerical scheme for tracking cyclone centres from
digital data. Part I: Development and operation of the scheme. Australian
Meteorological Magazine, 39, 155166.
Murray, R. J., and I. Simmonds, 1991: A
numerical scheme for tracking cyclone centres from
digital data. Part II: Application to January and July general circulation
model simulations. Australian Meteorological Magazine, 39, 167180.
Jones, D.A., and I. Simmonds, 1993: A climatology of Southern Hemisphere extratropical cyclones.
Climate Dynamics, 9, 131145.
Jones, D.A., and
Jones, D.A., 1994. An
objective study of Southern Hemisphere synoptic activity. PhD Thesis,
Simmonds,
Simmonds,
Simmonds,
Simmonds,
Simmonds,
Keable, M., I. Simmonds and K. Keay, 2002: Distribution and
temporal variability of 500 hPa cyclone
characteristics in the Southern Hemisphere. International
Journal of Climatology, 22,131-150.
Simmonds,
Simmonds,
Simmonds,
Lim, E.-P., 2005: Global changes in synoptic activity
with increasing atmospheric CO2. PhD Thesis,
Pezza, A. B., and I. Simmonds, 2005: The first
Simmonds,
Wassermann, S., C. Schmitt, C. Kottmeier
and I. Simmonds, 2006: Coincident vortices in Antarctic wind fields and sea ice
motion. Geophysical Research Letters, 33, L15810, doi:10.1029/2006GL026005.
White, W. B., and I. Simmonds, 2006: Sea surface
temperature-induced cyclogenesis in the Antarctic
circumpolar wave. Journal of Geophysical Research, 111, C08011,
doi:10.1029/2004JC002395.
Krinner, G., O. Magand,
Lim, E.-P., and I. Simmonds, 2007: Southern Hemisphere
winter extratropical cyclone characteristics and vertical organization observed
with the ERA-40 reanalysis data in 1979-2001. Journal of Climate, 20,
2675-2690.
Last Update: March 29 2008
Maintained by: Kevin Keay