Bay of Bengal Intraseasonal Oscillations and the 2018 Monsoon Onset
نویسندگان
چکیده
Abstract In the Bay of Bengal, warm, dry boreal spring concludes with onset summer monsoon and accompanying southwesterly winds, heavy rains, variable air–sea fluxes. Here, we summarize 2018 using observations collected through multinational Monsoon Intraseasonal Oscillations in Bengal (MISO-BoB) program between United States, India, Sri Lanka. MISO-BoB aims to improve understanding intraseasonal variability, field effort captured coupled response during a transition from active-to-break conditions central BoB. The active phase ∼20-day research cruise was characterized by warm sea surface temperature (SST > 30°C), cold atmospheric outflows intermittent rainfall, increasing winds (from 2 15 m s −1 ). Accumulated rainfall exceeded 200 mm 90% precipitation occurring first week. following break period both clear, persistent 10–12 wind evaporation 0.2 h . evolving environmental state included deepening ocean mixed layer ∼20 50 m), cooling SST (by ∼1°C), warming/drying lower midtroposphere. Local development consistent phasing large-scale oscillation. upper stores significant heat BoB, enough maintain above 29°C despite fluxes mixing. Comparison reanalysis indicates biases fluxes, which may be related overly cool prescribed SST. Resolution such offers path toward improved forecasting periods monsoon.
منابع مشابه
Intraseasonal variability of sea surface height in the Bay of Bengal
[1] Intraseasonal variability (ISV) of sea surface height (SSH) over the Bay of Bengal (BoB) is studied using altimetry data and an eddy-resolving ocean model. In both the model hindcast and satellite observations, large SSH ISV is found along the eastern and northern coasts of the BoB, in the western BoB, and in a zonal band across the Bay centered near 5 N. The ISV displays a clear seasonalit...
متن کاملA numerical investigation of the phytoplankton bloom in the Bay of Bengal during Northeast Monsoon
[1] A 4.5-layer model of the Indian Ocean coupled to a four-component (NPZD) ecosystem model is used to study the phytoplankton bloom in the Bay of Bengal during the Northeast Monsoon of 1996. The model realistically simulates the surface chlorophyll bloom observed by satellite-derived ocean-color images in the western Bay of Bengal during that time. It also reproduces the subsurface chlorophyl...
متن کاملTrace metal dynamics in zooplankton from the Bay of Bengal during summer monsoon.
Trace metal (Fe, Co, Ni, Cu, Zn, Cd, and Pb) concentrations in zooplankton from the mixed layer were investigated at 8 coastal and 20 offshore stations in the western Bay of Bengal during the summer monsoon of 2003. The ecotoxicological importance of trace metal uptake was apparent within the Bay of Bengal zooplankton. There was a distinct spatial heterogeneity of metals, with highest concentra...
متن کاملInteractions 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 کاملBuoy data assimilation to improve wave height assessment in Bay of Bengal during monsoon seasons
Significant wave height assessment in Bay of Bengal derived from third generation Wave Model (WAM cycle 4) has been improved by assimilating with continuous three hourly data from five moored buoys of National Institute of Ocean Technology using optimum interpolation technique. Covariance based weight function (gain) used in the study captures the model physics behind wind-wave process while di...
متن کاملذخیره 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: Bulletin of the American Meteorological Society
سال: 2021
ISSN: ['1520-0477', '0003-0007']
DOI: https://doi.org/10.1175/bams-d-20-0113.1