The intraseasonal fluctuation of Indian summer monsoon rainfall and its relation with monsoon intraseasonal oscillation (MISO) and Madden Julian oscillation (MJO)

نویسندگان

چکیده

The intraseasonal fluctuations of Indian summer monsoon rainfall (ISMR) are mainly controlled by northward propagating oscillation (MISO) and eastward Madden Julian (MJO). In the current study, we examine relationship between (active break spells) ISMR with phase propagation amplitude MISO MJO. We notice that active spells generally occur during phases 2–5 (MJO 3–6), 6–8 1). association active/break is more prominent than MJO phases. show composite unfiltered regression-based reconstructed for eight phases, which consistent earlier findings. field shows a systematic well-organised compared to field. Phase also indicates lead-lag robust composite. explained percentage variance reference 20–90-day filtered rainfall. It found long (> 7 days) predominantly occurs when either or MJO, both them active, associated signal somewhere in 2 5. A (MISO MJO) at least one (MJO/MISO) feeble, even though signals strong, they primarily located 1, 6, 8.

برای دانلود باید عضویت طلایی داشته باشید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Interactions between the summer mean monsoon and the intraseasonal oscillation in the Indian monsoon region

[1] The relationship between interannual variations of the seasonal mean monsoon and intraseasonal oscillation (ISO) during boreal summer over the Indian monsoon region is investigated. The result shows a negative correlation between all-India summer monsoon rainfall and the ISO intensity. It is argued that the negative correlation is primarily attributed to the impact of the mean state of Indi...

متن کامل

Northern Hemisphere Summer Monsoon Singularities and Climatological Intraseasonal Oscillation

Using climatological pentad mean outgoing longwave radiation (OLR) and European Centre for MediumRange Weather Forecasts analysis winds, the authors show that the Northern Hemisphere summer monsoon displays statistically significant climatological intraseasonal oscillations (CISOs). The extreme phases of CISO characterize monsoon singularities—monsoon events that occur on a fixed pentad with us...

متن کامل

Intraseasonal isotopic variation associated with the Madden‐Julian Oscillation

[1] The Madden‐Julian Oscillation (MJO) is the dominant mode of intraseasonal variability in the tropical atmosphere. This study examines the evolution of the hydrologic regime from before the onset of the MJO (pre‐onset period) to the MJO onset period, using deuterated water vapor (HDO) measurements from the Tropospheric Emission Spectrometer (TES) and from ground‐based stations. Ground‐based ...

متن کامل

Extremes of the Indian summer monsoon rainfall, ENSO and equatorial Indian Ocean oscillation

[1] It is well known that anomalies of the Indian Summer Monsoon Rainfall (ISMR) are linked to El Niño and Southern Oscillation (ENSO). We show that large anomalies of the ISMR are also linked to the Equatorial Indian Ocean Oscillation (EQUINOO) between states with enhancement/suppression of atmospheric convection over the western part of the equatorial Indian Ocean with suppression/enhancement...

متن کامل

Madden-Julian Oscillation analog and intraseasonal variability in a multicloud model above the equator.

The Madden-Julian Oscillation (MJO) is the dominant component of tropical intraseasonal variability, and a theory explaining its structure and successful numerical simulation remains a major challenge. A successful model for the MJO should have a propagation speed of 4-7 m/s predicted by theory; a wavenumber-2 or -3 structure for the planetary-scale, low-frequency envelope with distinct active ...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Theoretical and Applied Climatology

سال: 2022

ISSN: ['1434-4483', '0177-798X']

DOI: https://doi.org/10.1007/s00704-022-03970-4