Unusual ocean‐atmosphere conditions in the tropical Indian Ocean during 1994

@article{Behera1999UnusualOC,
  title={Unusual ocean‐atmosphere conditions in the tropical Indian Ocean during 1994},
  author={Swadhin K. Behera and Raghavan Krishnan and Toshio Yamagata},
  journal={Geophysical Research Letters},
  year={1999},
  volume={26}
}
The southeastern tropical Indian Ocean (SETIO) was characterized by unusually cold sea surface temperature (SST) and strong northwestward alongshore surface winds during 1994. Using multi‐source data sets including ocean model simulation, two key processes are identified for the SETIO cooling. Entrainment cooling produced most of the negative SST anomaly near the coast whereas evaporative cooling dominated the process away from the coast. Convection was anomalously suppressed over SETIO and the… 

Figures from this paper

Contributions of Indian Ocean Sea Surface Temperatures to Enhanced East African Rainfall

Abstract Links between extreme wet conditions over East Africa and Indian Ocean sea surface temperatures (SST) are investigated during the core of the so-called short rain season in October–November.

Thermocline Warming Induced Extreme Indian Ocean Dipole in 2019

The 2019 positive Indian Ocean Dipole (IOD) was the strongest event since the 1960s which developed independently without coinciding El Niño. The dynamics is not fully understood. Here we show that

The Indian Ocean SST dipole simulated in a coupled general circulation model

We are successful in simulating the recently discovered ocean‐atmosphere coupled phenomenon called the Indian Ocean Dipole for the first time, using a coupled general circulation model without flux

The Role of the Local Hadley Circulation over the Western Pacific on the Zonally Asymmetric Anomalies over the Indian Ocean

The onset processes of the zonally asymmetric anomalies of convection and sea surface temperature (SST) over the tropical Indian Ocean are investigated with considering seasonal evolution, and

Indian Ocean Dipolelike Variability in the CSIRO Mark 3 Coupled Climate Model

Abstract Coupled ocean–atmosphere variability in the tropical Indian Ocean is explored with a multicentury integration of the Commonwealth Scientific and Industrial Research Organisation (CSIRO) Mark

Interannual variability in the tropical Indian Ocean

[1] The interannual variability in the tropical Indian Ocean is examined using 41-year (1958–1998) seasonal anomalies of the upper-ocean heat content (HCA), sea surface temperature (SSTA), and

Pacific Ocean origin for the 2009 Indian summer monsoon failure

The Indian subcontinent suffered from a severe drought during the summer monsoon season of 2009 when El Niño‐like conditions evolved in the Pacific. The warm sea surface temperature (SST) anomalies

Coupled Ocean‐Atmosphere Variability in the Tropical Indian Ocean

The Indian Ocean Dipole (IOD) is a natural ocean-atmosphere coupled mode that plays important roles in seasonal and interannual climate variations. The coupled mode locked to boreal summer and fall

Simulation of SST fluctuations and circulation in the Equatorial Indian Ocean

Inter-annual variability in the equatorial Indian Ocean sometimes exhibits large Sea Surface Temperature (SST) fluctuations. The SST anomaly gradient between eastern and western equatorial Indian

Simulation of Interannual SST Variability in the Tropical Indian Ocean

Abstract A 2.5-layer thermodynamic ocean model is used to investigate interannual variability in sea surface temperature (SST) of the tropical Indian Ocean. Simulated SST agrees well with the data.
...

Response of the equatorial Indian Ocean to an unusual wind event during 1994

Unusual westward wind anomalies were observed in the Indian Ocean during 1994. The response of the ocean to these anomalies is studied using an ocean general circulation model forced with interannual

Simulation of Interannual SST Variability in the Tropical Indian Ocean

Abstract A 2.5-layer thermodynamic ocean model is used to investigate interannual variability in sea surface temperature (SST) of the tropical Indian Ocean. Simulated SST agrees well with the data.

Seasonal variations in the equatorial Indian Ocean and their impact on the Lombok throughflow

In order to identify the origin of the nonequilibrated pressure field which introduces semiannual variations to the Lombok throughflow, one of the major components of the Indonesian throughflow,

Forced Rossby waves in the southern tropical Indian Ocean

Seasonal and interannual variation of the upper southern tropical Indian Ocean (STIO) is described by harmonic and empirical orthogonal function (EOF) analysis of the depth of the 20°C isotherm (D20)

Global Water Vapor Flux and Maintenance during FGGE

Abstract The relative humidity, temperature and wind fields generated by the First Global GARP Experiment (FGGE) III-b analysis of the Geophysical Fluid Dynamics Laboratory (GFDL) are used to examine

Variation of Indonesian throughflow and the El Niño‐Southern Oscillation

The expendable bathythermograph (XBT) line Fremantle-Sunda Strait transects the eastern Indian Ocean between northwestern Australia and Java. It was established in 1983 with low-density sampling and

Water vapour budget and precipitation over the Arabian Sea during the northern summer

Water vapour budget of the lower troposphere over the Arabian Sea is studied by computing fluxes across the boundary walls of a rectangular volume around the Arabian Sea during September 1963 and

An Equatorial Jet in the Indian Ocean

  • K. Wyrtki
  • Environmental Science, Physics
    Science
  • 1973
A narrow, jet-like current flows eastward at high speed during both transition periods between the two monsoons, demonstrating that a time-variable current can have profound effects in changing the mass structure in the ocean.

The Relationship Between Eastern Equatorial Pacific Sea Surface Temperatures and Rainfall over India and Sri Lanka

Abstract Monsoon season (June–September) precipitation data from 31 Indian subdivisions and mean monthly precipitation data from 35 Indian and Sri Lanka stations, spanning the period 1875–79, were