Hawaiian rainfall is teleconnected to short-term climate variability in the Pacific Ocean. The summer Southern Oscillation Index (SOI) and summer sea-level pressure (SLP) over the North Pacific are used as predictors, and the following winter rainfall indices from three islands of Hawaii are used as
Long-range prediction of hawaiian winter rainfall using canonical correlation analysis
✍ Scribed by Pao-Shin Chu; Yuxiang He
- Publisher
- John Wiley and Sons
- Year
- 1994
- Tongue
- English
- Weight
- 745 KB
- Volume
- 14
- Category
- Article
- ISSN
- 0899-8418
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
Hawaiian rainfall is teleconnected to short‐term climate variability in the Pacific Ocean. The summer Southern Oscillation Index (SOI) and summer sea‐level pressure (SLP) over the North Pacific are used as predictors, and the following winter rainfall indices from three islands of Hawaii are used as predictands. To consolidate the large data array of the SLP field prior to prediction experiments, lagged correlation and empirical orthogonal function analyses are used.
Canonical correlation analysis has been used for predicting Hawaiian winter rainfall. Among many schemes tested, predictions. Cross‐validation techniques have also been used to estimate the “overall” forecast skill of various schemes, and the results are consistent with those from prediction experiments. Winter rainfall in Hawaii can be predicted with a good degree of success two seasons in advance using the summer SOI and the first four eigenmodes of summer SLP over the North Pacific as predictors.
📜 SIMILAR VOLUMES
A statistically based technique is used to study the variability and predictability of South African summer rainfall. The country is divided into homogeneous regions on the basis of the interannual rainfall variability. Canonical variates are then used to make 3-month aggregate precipitation forecas
Canonical correlation analysis (CCA) is used for predicting Mei-Yu (May±June) rainfall for eight major stations in Taiwan based on the antecedent November±December sea-surface temperatures (SSTs) over the Paci®c Ocean (50 N±40 S, 120 E± 90 W). To reduce the large dimensionality of the SST data set,
Inverse heteronuclear shift correlation via long-range coupling to the carbonyl carbons of the cyclic hexapeptide cyclo(-Phe1\*-Thr'o-AIa9-Trps-Phe7-D-Pro6-) allows the sequential assignment of the amino acids. This experiment has a higher sensitivity than the conventional COLOC sequence.