Zonal and meridional Seasoar sections centered at 1°50’S, 156°06’E were repeated >30 times in three 20-day periods between November 13, 1992, and February 15, 1993. Both sections were 130 km long, and sampling depth was 0–280 m, with a vertical resolution of ~2 dbar (2 x 104 Pa) and a horizontal resolution of ~3 km. The observed fields are complex and variable and are summarized graphically in several forms. Characteristics of the near-surface layer varied with the local winds which were variable and weak (<6 m s-1) during the first 20-day period, strong and westerly (>10 m s-1) during much of the second, and moderate and westerly (4-10 m s-1) during most of the third. Near-surface temperatures were warmest (up to 30°C) during the first per...
AXCTD and AXBT data used for this study are available at http://data.eol.ucar.edu/ master_list/?proj...
Abstract. Mooring measurements at 0 ø, 165øE, for the period November 1988 to August 1991 indicate t...
Because of the relatively calm winds which prevail over the western Pacific warm pool, the diurnal c...
From December 1992 to February 1993, 18 meridional sections of temperature, salinity, and current we...
Moored current and temperature measurements were recorded simultaneously for 2 years (August 1932-Ju...
This paper presents the results of an experiment in the western equatorial Pacific centered on the e...
ridional sections of temperature, salinity, and current were col-lected along 156"E, from 5&quo...
High-resolution measurements of temperature and salinity were made in the near-surface layer of the ...
In this study, the processes affecting sea surface temperature variability over the 1992–98 period, ...
The air-sea interaction thermodynamics of the western equatorial Pacific, the Earth\u27s largest reg...
In this study, the processes affecting sea surface temperature variability over the 1992–98 period, ...
The thermocline is defined as the ocean layer for which the vertical thermal gradient is maximum. In...
Abstract Seasonal variations of the upper ocean, such as mixed layer depth (MLD) and sea surface tem...
Thesis (Ph. D.)--University of Hawaii at Manoa, 1993.Microfiche.xvii, 190 leaves, bound 29 cmProcess...
A westerly wind burst observed in the warm pool of the western equatorial Pacific Ocean cooled the o...
AXCTD and AXBT data used for this study are available at http://data.eol.ucar.edu/ master_list/?proj...
Abstract. Mooring measurements at 0 ø, 165øE, for the period November 1988 to August 1991 indicate t...
Because of the relatively calm winds which prevail over the western Pacific warm pool, the diurnal c...
From December 1992 to February 1993, 18 meridional sections of temperature, salinity, and current we...
Moored current and temperature measurements were recorded simultaneously for 2 years (August 1932-Ju...
This paper presents the results of an experiment in the western equatorial Pacific centered on the e...
ridional sections of temperature, salinity, and current were col-lected along 156"E, from 5&quo...
High-resolution measurements of temperature and salinity were made in the near-surface layer of the ...
In this study, the processes affecting sea surface temperature variability over the 1992–98 period, ...
The air-sea interaction thermodynamics of the western equatorial Pacific, the Earth\u27s largest reg...
In this study, the processes affecting sea surface temperature variability over the 1992–98 period, ...
The thermocline is defined as the ocean layer for which the vertical thermal gradient is maximum. In...
Abstract Seasonal variations of the upper ocean, such as mixed layer depth (MLD) and sea surface tem...
Thesis (Ph. D.)--University of Hawaii at Manoa, 1993.Microfiche.xvii, 190 leaves, bound 29 cmProcess...
A westerly wind burst observed in the warm pool of the western equatorial Pacific Ocean cooled the o...
AXCTD and AXBT data used for this study are available at http://data.eol.ucar.edu/ master_list/?proj...
Abstract. Mooring measurements at 0 ø, 165øE, for the period November 1988 to August 1991 indicate t...
Because of the relatively calm winds which prevail over the western Pacific warm pool, the diurnal c...