2011•Unpublished venueRequires access

Study on the relationship between ENSO and tropical Indian Ocean temperature

Li Hai

Open publisher page 1 citations

Abstract

The relationship between ENSO and Indian Ocean Dipole was discussed by using the data set of sea temperature from Scripps Institute of Oceanography,the air temperature at 1000hPa from the NCEP reanalysis data and the Nino3 index from the Climate Prediction Center(CPC) of U.S.A.during the period from 1955 to 2001.The results show that there exists a Dipole on the maximum temperature anomalous level(MTAL) in the Indian Ocean,which close relates to ENSO in the Pacific Ocean.During El Nino periods there are good relationships between ENSO and Indian Ocean Dipole which maximum correlation occurring when ENSO leads by one month,but in La Nina periods the relationship is not so good.The distribution of Dipole in Indian Ocean is from northeast to southwest,which one(west) pole in 65oE-75oE,6oS-10oS and the other in 85oE-95oE,2oN-6oN,which is different from that defined by Saij.The correlation coefficients of Nino3 index with temperature anomalies in the west/east poles on the MTAL are over 0.4-0.15,respectively.It is a main sea temperature system in the tropical Indian Ocean.However,in the surface layer from sea surface to the depth of 20 m-30 m there is no such a dipole with opposite sea temperature anomalies in the NE and SW of tropical Indian Ocean.The SSTA in the NE might be influenced by the sensible exchange process because the evolution of sea and 1 000 hPa air temperature anomaly time series of the NE of tropical Indian Ocean is quite similar except those during 1962-1963 and 1986.The periods of Indian Ocean Dipole are shorter than that of ENSO,and about 1 to 6-year.

About this research paper

What this paper is about

The relationship between ENSO and Indian Ocean Dipole was discussed by using the data set of sea temperature from Scripps Institute of Oceanography,the air temperature at 1000hPa from the NCEP reanalysis data and the Nino3 index from the Climate Prediction Center(CPC) of U.S.A.during the period from 1955 to 2001.The results show that there exists a Dipole on the maximum temperature anomalous level(MTAL) in the Indian Ocean,which close relates to ENSO in the Pacific Ocean.During El Nino periods there are good relationships between ENSO and Indian Ocean Dipole which maximum correlation occurring when ENSO leads by one month,but in La Nina periods the relationship is not so good.The distribution of Dipole in Indian Ocean is from northeast to southwest,which one(west) pole in 65oE-75oE,6oS-10oS and the other in 85oE-95oE,2oN-6oN,which is different from that defined by Saij.The correlation coefficients of Nino3 index with temperature anomalies in the west/east poles on the MTAL are over 0.4-0.15,respectively.It is a main sea temperature system in the tropical Indian Ocean.However,in the surface layer from sea surface to the depth of 20 m-30 m there is no such a dipole with opposite sea temperature anomalies in the NE and SW of tropical Indian Ocean.The SSTA in the NE might be influenced by the sensible exchange process because the evolution of sea and 1 000 hPa air temperature anomaly time series of the NE of tropical Indian Ocean is quite similar except those during 1962-1963 and 1986.The periods of Indian Ocean Dipole are shorter than that of ENSO,and about 1 to 6-year.

Why it matters

OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The relationship between ENSO and Indian Ocean Dipole was discussed by using the data set of sea temperature from Scripps Institute of Oceanography,the air temperature at 1000hPa from the NCEP reanalysis data and the Nino3 index from the Climate Prediction Center(CPC) of U.S.A.during the period from 1955 to 2001.The results show that there exists a Dipole on the maximum temperature anomalous level(MTAL) in the Indian Ocean,which close relates to ENSO in the Pacific Ocean.During El Nino periods there are good relationships between ENSO and Indian Ocean Dipole which maximum correlation occurring when ENSO leads by one month,but in La Nina periods the relationship is not so good.The distribution of Dipole in Indian Ocean is from northeast to southwest,which one(west) pole in 65oE-75oE,6oS-10oS and the other in 85oE-95oE,2oN-6oN,which is different from that defined by Saij.The correlation coefficients of Nino3 index with temperature anomalies in the west/east poles on the MTAL are over 0.4-0.15,respectively.It is a main sea temperature system in the tropical Indian Ocean.However,in the surface layer from sea surface to the depth of 20 m-30 m there is no such a dipole with opposite sea temperature anomalies in the NE and SW of tropical Indian Ocean.The SSTA in the NE might be influenced by the sensible exchange process because the evolution of sea and 1 000 hPa air temperature anomaly time series of the NE of tropical Indian Ocean is quite similar except those during 1962-1963 and 1986.The periods of Indian Ocean Dipole are shorter than that of ENSO,and about 1 to 6-year.

Key concepts: Subtropical Indian Ocean Dipole, Sea surface temperature, La Niña, Indian Ocean Dipole, Climatology, El Niño Southern Oscillation, Indian ocean, Anomaly (physics)

Related papers

Back to paper searchBrowse research topicsOriginal source
Study on the relationship between ENSO and tropical Indian Ocean temperature — Research Paper | ScholarLens