Related Experiment Video
Updated: Jul 4, 2025

Measuring the Structure, Composition, and Change of Underwater Environments with Large-area Imaging
Published on: April 18, 2025
Aircraft observations in a tropical supercluster over the equatorial Indian Ocean during MISO-BOB field campaign
Jayesh Phadtare1, Harindra J S Fernando2,3, Garrett Black4
1Department of Civil and Environmental Engineering and Earth Sciences, University of Notre Dame, Notre Dame, IN, 46556, USA. jayesh.phadtare@gmail.com.
Abstract:
The Monsoon Intra-Seasonal Oscillations in the Bay of Bengal (MISO-BOB) field campaign was conducted in the Indian Ocean during the 2018 and 2019 summer monsoon seasons. WC-130J aircraft of the 53rd Weather Reconnaissance Squadron of the US Air Force participated in the campaign in June 2018. The dropsonde observations across a tropical supercluster showed zonal wind variations in association with the structure of the convectively coupled Kelvin wave (CCKW). Within the supercluster, easterlies (westerlies) were observed in the upper (lower) troposphere; this transformation occurred just below the 0[Formula: see text] C level. The cold pool had an easterly component throughout, and it was coldest (by 2.5[Formula: see text] C) at the center of the supercluster, deepest ([Formula: see text] [Formula: see text]) at its rear/western end, and shallowest ([Formula: see text] 300 m) at the front/eastern end. The level of free convection (LFC) at the front end was at [Formula: see text] altitude. At the eastern flank of the supercluster, zonal convergence in the lower troposphere occurred between 500-1500 m levels above the surface between the westerlies within the supercluster and opposing ambient easterlies. Thus, the uplifting of conditionally unstable air parcels above LFC to the east of the supercluster was likely to occur due to this convergence rather than the cold pool influence. Conversely, the western flank of the supercluster had low-level zonal divergence. These observations support the notion of 'self-similarity' among the mesoscale convective systems and large-scale waves.
Related Concept Videos
Boundary Layer Characteristics
Cluster Sampling Method
To choose a cluster sample, divide the population into clusters (groups) and then randomly select some of the clusters. All the members from these clusters are in the cluster sample. For example, if you randomly sample four departments from your...
Precipitation Gravimetry
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Data Collection by Observations
An astronomer viewing the motion and brightness of stars in the sky and recording the data is an example of observational data collection. A botanist recording...
General External Flow Characteristics
Atomic Emission Spectroscopy: Instrumentation

