ML4WX

Sub-seasonal to seasonal

Week 3–4 Prediction of Wintertime CONUS Temperature Using Machine Learning Techniques

Paul Buchmann, Timothy DelSole

Frontiers in Climate ·

PaperPDF

In one sentence. Ridge and lasso models using Niño3.4 give modest week 3-4 skill for US winter temperature, only slightly beating CFSv2 and climatology-based baselines.

Abstract

This paper shows that skillful week 3–4 predictions of a large-scale pattern of 2 m temperature over the US can be made based on the Nino3.4 index alone, where skillful is defined to be better than climatology. To find more skillful regression models, this paper explores various machine learning strategies (e.g., ridge regression and lasso), including those trained on observations and on climate model output. It is found that regression models trained on climate model output yield more skillful predictions than regression models trained on observations, presumably because of the larger training sample. Nevertheless, the skill of the best machine learning models are only modestly better than ordinary least squares based on the Nino3.4 index. Importantly, this fact is difficult to infer from the parameters of the machine learning model because very different parameter sets can produce virtually identical predictions. For this reason, attempts to interpret the source of predictability from the machine learning model can be very misleading. The skill of machine learning models also are compared to those of a fully coupled dynamical model, CFSv2. The results depend on the skill measure: for mean square error, the dynamical model is slightly worse than the machine learning models; for correlation skill, the dynamical model is only modestly better than machine learning models or the Nino3.4 index. In summary, the best predictions of the large-scale pattern come from machine learning models trained on long climate simulations, but the skill is only modestly better than predictions based on the Nino3.4 index alone.

Labels

Topic
Sub-seasonal to seasonal, Post-processing & calibration
Type
Evaluation or intercomparison of existing models
Method
Classical ML (trees, GP, linear, kernels)
Time scale
2 weeks–2 months
Domain
Regional
Data
CMIP / climate model output, NWP analysis or forecasts (IFS, GFS, ...)
Status
Research
Identifiers
DOI:10.3389/fclim.2021.697423 OpenAlex:W3208736825
Added
2026-10-22

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