**Abstract** Changes in North Atlantic sea surface temperature (SST) are regarded as a key element of the climate during the Quaternary. However, there are relatively few longβterm records providing quantitative SST estimates from this region. Using planktic foraminiferalβderived SSTs together with
The surface Temperature of the North Atlantic during 1911
β Scribed by M. W. Campbell Hepworth
- Publisher
- John Wiley and Sons
- Year
- 1912
- Tongue
- English
- Weight
- 239 KB
- Volume
- 5
- Category
- Article
- ISSN
- 1434-2944
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
## Abstract Based on generated time series of the central pressure of the subtropical high, the behaviour of this atmospheric centre of action has been examined since 1950 with regard to the interβannual variations, persistence, linear trends, abrupt change, spectral analysis and interactions. The
Correlation-matrix principal components of North Atlantic sea-surface temperature anomalies for the interval 1950Β±1970 account for the anomalous variability observed during the interval 1972Β±1992 better than do similar numbers of covariancematrix principal components, regional averages, or carefully