The Challenge of Weather and Climate Prediction

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Meteorology".

Deadline for manuscript submissions: 28 June 2024 | Viewed by 996

Special Issue Editors


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Guest Editor
Retired, previously Croatian Meteorological and Hydrological Service, 10000 Zagreb, Croatia
Interests: data assimilation methods for numerical weather prediction; ensemble forecasts; seasonal and climate forecasting; verification of weather and climate forecasting and outlooks
Special Issues, Collections and Topics in MDPI journals

E-Mail Website
Guest Editor
Head of Data Processing and Management Department, Croatian Meteorological and Hydrological Service, Ravnice 48, 10000 Zagreb, Croatia
Interests: boundary-layer meteorology (application of Monin–Obukhov similarity theory for the wind speed estimation in the lower part of the atmospheric surface layer)
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Weather and climate prediction (forecasting) are among the greatest challenges faced in theoretical and applied atmospheric science. Both require comprehensive theoretical knowledge and extensive operational systems. The first successful numerical weather forecast for one day in advance was obtained in the 1950s, when computers began to operate and so-called filtered atmospheric models were utilized. During the 1990s, a so-called global primitive equation atmospheric model was employed; this was operational after the application of a specific data assimilation procedure. Very soon after that, the application of coupled atmosphere and ocean models  resulted in the prolongation of the forecasting period up to five or six days in advance. Unfortunately, due to the presence of deterministic chaos in the atmosphere–ocean dynamic system, long-range forecasting is limited. Ensemble forecasting is a useful probabilistic component of the forecasting system as it is able to inform us of the reliability of medium-range weather forecasting. As time goes on, the reliability decreases; thus, after 10 days, medium-range weather forecasts are considered non-reliable. However, if atmosphere–ocean global models are considered as boundary condition problems instead of as initial condition problems, then useful seasonal and even centennial outlooks can be achieved, but with “condensed” products. Determining the limitations of weather and climate forecasting can be achieved by comparing forecasts with real observations, i.e., via forecast verification.  

Dr. Kreso Pandzic
Dr. Tanja Likso
Guest Editors

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Keywords

  • data assimilation for numerical weather and climate forecasting
  • application of atmospheric and oceanic models
  • ensemble forecasting
  • weather and climate forecasting verification.

Published Papers (1 paper)

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Research

23 pages, 4474 KiB  
Article
Development and Evaluation of a Short-Term Ensemble Forecasting Model on Sea Surface Wind and Waves across the Bohai and Yellow Sea
by Tonghui Zang, Jing Zou, Yunzhou Li, Zhijin Qiu, Bo Wang, Chaoran Cui, Zhiqian Li, Tong Hu and Yanping Guo
Atmosphere 2024, 15(2), 197; https://doi.org/10.3390/atmos15020197 - 04 Feb 2024
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Abstract
In this study, an ensemble forecasting model for in situ wind speed and wave height was developed using the Coupled Ocean–Atmosphere–Wave–Sediment Transport (COAWST) model. This model utilized four bias correction algorithms—Model Output Statistics (MOS), Back Propagation Neural Network (BPNN), Long Short-Term Memory (LSTM) [...] Read more.
In this study, an ensemble forecasting model for in situ wind speed and wave height was developed using the Coupled Ocean–Atmosphere–Wave–Sediment Transport (COAWST) model. This model utilized four bias correction algorithms—Model Output Statistics (MOS), Back Propagation Neural Network (BPNN), Long Short-Term Memory (LSTM) neural network, and Convolutional Neural Network (CNN)—to construct ensemble forecasts. The training data were derived from the COAWST simulations of one year and observations from three buoy stations (Laohutan, Zhifudao, and Lianyungang) in the Yellow Sea and Bohai Sea. After the optimization of the bias correction model training, the subsequent evaluations on the ensemble forecasts showed that the in situ forecasting accuracy of wind speed and wave height was significantly improved. Although there were some uncertainties on bias correction performance levels for individual algorithms, the uncertainties were greatly reduced by the ensemble forecasts. Depending on the dynamic weight assignment, the ensemble forecasts presented a stable performance even when the corrected forecasts by three algorithms had an obvious negative bias. Specifically, the ensemble forecasting bias was found with a mean reduction of about 96%~99% and 91%~95% for wind speed and wave height, and a reduction of about 91%~98% and 16%~54% during the period of Typhoon “Muifa”. For the four correction algorithms, the performance of bias correction was not directly related to the algorithm complexity. However, the strategies with more complex algorithms (i.e., CNN) were more conservative, and simple algorithms (i.e., MOS) might have induced unstable performance levels despite their lower bias in some cases. Full article
(This article belongs to the Special Issue The Challenge of Weather and Climate Prediction)
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