May 17, 2016:2015 data was added for the AL, EP and CP basins.
November 5, 2015: 2014 data was added for the AL, EP and CP basins.
September 11, 2014: Atlantic, Central and Eastern Pacific files updated with 2013 cases.
January 7, 2014: Southern hemisphere and North Indian Ocean diagnostic files added to the developmental data.
May 10, 2013: Central and East Pacific files now separated. Atlantic, East Pacific, Central Pacific and Western Pacific files updated with 2012 cases.
September 4, 2012: West Pacific developmental data file now available for 2000 - 2011.
Tropical cyclone (TC) track forecast errors have decreased considerably over the past several decades. However, there have been only modest intensity forecast improvements. Because of the complex physical processes affecting intensity changes, statistical forecast models have remained competitive with much more general prediction systems. For this reason, the National Hurricane Center (NHC) continues to run a hierarchy of operational intensity models that range from the simple Statistical Hurricane Intensity Prediction Scheme (SHIPS) to the fully coupled atmosphere-ocean Hurricane Weather Research and Forecast (HWRF) system. Several projects are underway at CIRA and RAMMB to improve the SHIPS and related statistical intensity forecast models. This web page provides a summary of this work and links to publications and datasets used in this research.
The original motivation for the SHIPS model began in 1988 when John Kaplan from the Hurricane Research Division (HRD) participated in a visiting forecaster program at NHC during Hurricane Joan. It quickly became apparent that NHC had very little objective guidance for intensity prediction, so John worked with Mark DeMaria (also from HRD at that time) on a new project that led to the development of the Statistical Hurricane Intensity Prediction Scheme (SHIPS). The SHIPS model built on a previous effort at statistical intensity forecasting by Bob Merrill, and combines predictors from climatology, persistence, the atmosphere and ocean to estimate changes in the maximum sustained surface winds of tropical cyclones. The first real time runs of SHIPS were performed in 1990, and only provided forecasts to 48 hrs at 00 and 12 UTC. The output was available to NHC only in hardcopy format. Beginning in 1991, the digital forecasts were saved the Automated Tropical Cyclone Forecast (ATCF) A-decks, and are available from NHC’s archive at ftp://ftp.nhc.noaa.gov/atcf/archive . The model name in the ATCF is SHIP for the version without land effects (since 1991), DSHP for the version with land effects (since 2000) and LGEM for a related logistic growth equation model (since 2006). For the three year period 1996-1998, the ATCF model name for SHIP was changed to LBAR, which provided the track forecast for SHIPS at that time.
The original SHIPS model was "statistical-synoptic" where no information from large-scale forecast models were used. (all synoptic predictors were from model analyses) The model was converted to a "statistical-dynamical" model in 1997, where predictors were obtained from atmospheric forecast models, in addition to analyses. Table 1 shows a summary of the major milestones in the SHIPS and related models.
Although SHIPS forecasts since about 1997 have shown some skill compared to climatology and persistence forecasts, they have not performed well for rapidly intensifying cases. For this reason, the rapid intensity index (RII) was developed to provide an estimate of the probability of rapid intensification in the next 24 hr. The RII probabilities are provided as part of the SHIPS model text file, and use a subset of the SHIPS predictors most related to rapid intensification in a discriminant analysis algorithm. The SHIPS model provides intensity forecasts for the Atlantic, eastern and central North Pacific. A similar model called the Statistical Typhoon Intensity Prediction Scheme (STIPS) was developed for the western North Pacific, and later for the Indian Ocean and southern hemisphere.
The SHIPS and STIPS models use a linear regression technique, with the impacts of land applied as a correction in a post-processing step. To overcome some of the limitations of this formulation, the Logistic Growth Equation Model (LGEM) was developed. LGEM uses a simple nonlinear differential equation commonly used to model population growth to forecast intensity changes. LGEM is more sensitive to time variations in the predictors, and overcomes some of the limitations of the linear assumptions in the SHIPS model.
LGEM can be run with a much smaller number of predictors than SHIPS. A 2-predictor version is under development that provides a simple phase-space interpretation of the results. Further details are available here.
Current research involves improving SHIPS, LGEM and RII by better utilizing GOES imagery, new information from satellite-based total precipitable water products, and surface flux estimates. Methods for using the adjoint of the LGEM model to better include persistence are also under development. Lightning data is also being examined for possible use in SHIPS, LGEM and RII. The projects are partially sponsored by the Joint Hurricane Testbed (JHT), GOES-R Risk Reduction Program and Hurricane Forecast Improvement Project (HFIP).
Milestones in the Operational SHIPS and Related Model Development
- 1990 - First real-time runs of SHIPS for the Atlantic
- 1991 - Intensity forecasts to 72 h written to ATCF
- 1996 - East Pacific SHIPS developed and processing moved from HRD to NHC
- 1997 - Model converted from "statistical-synoptic" to "statistical-dynamical"
- 2000 - Decay component added to account for land effects (D-SHIPS)
- 2001 - Forecasts extended from 3 to 5 days, predictors from NCEP global model
- 2003 - Rapid intensification index added for Atlantic
- 2003 - STIPS model for the western North Pacific
- 2004 - Oceanic heat content predictor added to Atlantic model
- 2004 - GOES infrared predictors added to Atlantic and east Pacific models
- 2004 - Rapid intensification index added for east Pacific
- 2005 - STIPS model for the Indian Ocean and southern hemisphere
- 2006 - Logistic Growth Equation Model formulation added to SHIPS processing
- 2009 - Oceanic heat content predictor added to east Pacific model
- 2011 - Storm type classification (tropical, subtropical, extratropical) algorithm added
- 2013 - Versions of SHIPS and LGEM developed for the western North Pacific, Indian Ocean and Southern Hemisphere
- 2013 - Basic versions of the rapid intensification index (30 kt threshold for 24 hr) developed for the western North Pacific, Indian Ocean and Southern Hemisphere
Disclaimer: These environmental data and related items of information have not been formally disseminated by NOAA and do not represent and should not be construed to represent any agency determination, view, or policy.