Download presentation
Presentation is loading. Please wait.
Published byΑἴαξ Ζάνος Modified over 6 years ago
1
Improving forecasts through rapid updating of temperature trajectories and statistical post-processing Nina Schuhen, Thordis L. Thorarinsdottir and Alex Lenkoski
2
Status quo Forecasts are not revisited once issued
Newest forecast run is usually the best Idea: correct a forecast trajectory while it verifies
3
More skill!
4
Data set: UK Met Office MOGREPS-UK 2.2 km 70 Levels
36 hourly forecast 4 times/day 12 members Interpolated to 149 observation sites in UK and Ireland Training period: Jan to Dec 2014 Evaluation period: Jan 2015 to Jul 2016 Surface temperature
5
EMOS / NGR Raw ensemble output is calibrated using EMOS (NGR)
Removal of deterministic and probabilistic biases Performed after the ensemble run is completed, based on a rolling training period Gneiting, T., A.E. Raftery, A.H. Westveld, and T. Goldman, 2005: Calibrated Probabilistic Forecasting Using Ensemble Model Output Statistics and Minimum CRPS Estimation. Mon. Wea. Rev., 133, 1098–1118
6
Previous results for EMOS
7
EMOS / NGR Raw ensemble output is calibrated using EMOS (NGR)
Removal of deterministic and probabilistic biases Performed after the ensemble run is completed, based on a rolling training period 16% reduction in CRPS Here: correct EMOS mean, keep calibrated EMOS spread Gneiting, T., A.E. Raftery, A.H. Westveld, and T. Goldman, 2005: Calibrated Probabilistic Forecasting Using Ensemble Model Output Statistics and Minimum CRPS Estimation. Mon. Wea. Rev., 133, 1098–1118
8
Correction of forecast trajectories
We allow for 1 hour delay for measurements to be transmitted, processed, quality-controlled, etc. Here: 03 UTC run at Heathrow Airport Data analysis shows no systematic trend in forecast error Strong connection to diurnal cycle Regression approach is the most appropriate
9
Framework At any time a new forecast is issued for the next 36 hours: with Observations become available while this forecast trajectory is valid Compute forecast error at : Correct the next forecast(s) using a function of this error:
10
Forecast error correlation matrix
11
Regression method Estimate future errors by linear regression
Previous forecasts’ errors as predictors: Correct forecasts by adding the estimated error: Find earliest lead time, where is significantly different from 0
12
Length of error correction period
13
Development of forecast error
14
Development of forecast error
15
Development of forecast error
16
Extension to multiple sites
17
Conclusions Strong correlation between error at different lead times
Predictability depends heavily on the time of day Regression model reduces forecast error overall Big margin for short-term corrections Might prefer corrected forecasts from a previous model run to the first forecasts from the current one
18
Future work Investigate relationship between forecast runs
Develop rules for combining forecast runs to one «best» trajectory Take into account seasonal effects Kriging to spread regression parameters spatially? Extend to other weather parameters
19
Example
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.