MISMO FIELD EXPERIMENT IN THE EQUATORIAL INDIAN OCEAN

Kunio Yoneyama
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Yukio Masumoto
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Yoshifumi Kuroda
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Masaki Katsumata
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Keisuke Mizuno
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Yukari N. Takayabu
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Masanori Yoshizaki
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Ali Shareef
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Yasushi Fujiyoshi
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Michael J. McPhaden
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V. S. N. Murty
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Ryuichi Shirooka
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Kazuaki Yasunaga
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Hiroyuki Yamada
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Naoki Sato
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Tomoki Ushiyama
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Qoosaku Moteki
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Ayako Seiki
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Mikiko Fujita
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Kentaro Ando
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Hideaki Hase
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Iwao Ueki
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Takanori Horii
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Chie Yokoyama
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Tomoki Miyakawa
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The Mirai Indian Ocean cruise for the Study of the Madden-Julian oscillation (MJO)-convection Onset (MISMO) was a field experiment that took place in the central equatorial Indian Ocean during October–December 2006, using the research vessel Mirai, a moored buoy array, and landbased sites at the Maldive Islands. The aim of MISMO was to capture atmospheric and oceanic features in the equatorial Indian Ocean when convection in the MJO was initiated. This article describes details of the experiment as well as some selected early results.

Intensive observations using Doppler radar, radiosonde, surface meteorological measurements, and other instruments were conducted at 0°, 80.5°E, after deploying an array of surface and subsurface moorings around this site. The Mirai stayed within this buoy array area from 24 October through 25 November. After a period of stationary observations, underway meteorological measurements were continued from the Maldives to the eastern Indian Ocean in early December.

All observations were collected during an El Nino and a positive Indian Ocean Dipole (IOD) event, which tended to suppress convection in the western Pacific and eastern Indian Ocean in throughout much of November 2006. However, as the IOD began to wane in mid-November, an abrupt change from westerly to easterly took place in upper tropospheric winds in the MISMO study region. By late November and early December, deep convection developed over the central Indian Ocean and eastward movement of large-scale cloud systems were observed. This article describes these variations in detail and how they advance our understanding of the onset of tropical deep convection on intraseasonal time scales.

*National Institute of Oceanography, Contribution Number 4378.

IORGC, JAMSTEC, Yokosuka, Japan

IORGC, JAMSTEC, Yokosuka, and Department of Earth and Planetary Sciences, University of Tokyo, Tokyo, Japan

Marine Technology Center, JAMSTEC, Yokosuka, Japan

Center for Climate System Research, University of Tokyo, Kashiwa, and IORGC, JAMSTEC, Yokosuka, Japan

National Meteorological Center, Male, Maldives

Hokkaido University, Sapporo, Japan

Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, Washington

National Institute of Oceanography, Goa, India

Center for Climate System Research, University of Tokyo, Kashiwa, Japan

+,#CURRENT AFFILIATIONS: USHIYAMA—National Institute for Agro-Environmental Sciences, Tsukuba, Japan; KURODA—Nippon Marine Enterprises Ltd., Yokosuka, Japan

CORRESPONDING AUTHOR: Kunio Yoneyama, Institute of Observational Research for Global Change (IORGC)/Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15, Natsushima-cho, Yokosuka 237-0061, Japan E-mail: yoneyamak@jamstec.go.jp

The Mirai Indian Ocean cruise for the Study of the Madden-Julian oscillation (MJO)-convection Onset (MISMO) was a field experiment that took place in the central equatorial Indian Ocean during October–December 2006, using the research vessel Mirai, a moored buoy array, and landbased sites at the Maldive Islands. The aim of MISMO was to capture atmospheric and oceanic features in the equatorial Indian Ocean when convection in the MJO was initiated. This article describes details of the experiment as well as some selected early results.

Intensive observations using Doppler radar, radiosonde, surface meteorological measurements, and other instruments were conducted at 0°, 80.5°E, after deploying an array of surface and subsurface moorings around this site. The Mirai stayed within this buoy array area from 24 October through 25 November. After a period of stationary observations, underway meteorological measurements were continued from the Maldives to the eastern Indian Ocean in early December.

All observations were collected during an El Nino and a positive Indian Ocean Dipole (IOD) event, which tended to suppress convection in the western Pacific and eastern Indian Ocean in throughout much of November 2006. However, as the IOD began to wane in mid-November, an abrupt change from westerly to easterly took place in upper tropospheric winds in the MISMO study region. By late November and early December, deep convection developed over the central Indian Ocean and eastward movement of large-scale cloud systems were observed. This article describes these variations in detail and how they advance our understanding of the onset of tropical deep convection on intraseasonal time scales.

*National Institute of Oceanography, Contribution Number 4378.

IORGC, JAMSTEC, Yokosuka, Japan

IORGC, JAMSTEC, Yokosuka, and Department of Earth and Planetary Sciences, University of Tokyo, Tokyo, Japan

Marine Technology Center, JAMSTEC, Yokosuka, Japan

Center for Climate System Research, University of Tokyo, Kashiwa, and IORGC, JAMSTEC, Yokosuka, Japan

National Meteorological Center, Male, Maldives

Hokkaido University, Sapporo, Japan

Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, Washington

National Institute of Oceanography, Goa, India

Center for Climate System Research, University of Tokyo, Kashiwa, Japan

+,#CURRENT AFFILIATIONS: USHIYAMA—National Institute for Agro-Environmental Sciences, Tsukuba, Japan; KURODA—Nippon Marine Enterprises Ltd., Yokosuka, Japan

CORRESPONDING AUTHOR: Kunio Yoneyama, Institute of Observational Research for Global Change (IORGC)/Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15, Natsushima-cho, Yokosuka 237-0061, Japan E-mail: yoneyamak@jamstec.go.jp
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