The atmospheric budgets of mass, water vapor, heat, momentum, and mechanical energy have been analyzed for a 5-day undisturbed period (June 22-26, 1969) during the Barbados Oceanographic and Meteorological Experiment (BOMEX). Data were obtained from rawinsondes launched every 1% hr from the four corner ships of the BOMEX array. Computations were limited to the lowest 500 mb within a 500-km squa...

The study of ocean bottom pressure (OBP) helps to understand the changes in sea level budget and deep circulation. In this study, characteristics mechanisms interannual OBP variability Southern Indian Ocean are examined using Gravity Recovery Climate Experiment (GRACE) satellite data from 2003 2016. Results show that there two energetic centers (50°–60°S, 40°–60°E 45°–60°S, 80°–120°E). magnitud...

Abstract A model of the LOng‐RAnge Navigation signal can provide a mathematical for development related technology research. The propagation variations exhibit non‐stationary and non‐linear characteristics due to time‐varying nature atmospheric dielectric constant in channel. Dirichlet process mixtures method is used by authors statistical properties radio wave attenuation, Gibbs sampling flexi...

the present research article highlights the metal (cd, cu, pb, zn and fe)distribution pattern in the rspm generated in different hot spot sites located at kochi, thequeen of arabian sea. these sampling sites are categorized under three different zonesas estuarine, riverine, and coastal. two sampling phases are selected in order to check theconsistency in pollution trend after a two year gap and...

Composite large-scale dynamical fields contemporaneous with low cloud types observed at midlatitude Ocean Weather Station (OWS) C and eastern subtropical OWS N are used to establish representative relationships between low cloud type and the synoptic environment. The composites are constructed by averaging meteorological observations of surface wind and sea level pressure from volunteering obse...

Daily surface wind variations over the equatorial eastern Pacific Ocean during summer 1992 are documented, using hourly observations from the tropical atmosphere ocean moored buoy array. Diurnal and semidiurnal variations are apparent in the zonal wind component, with peak-to-peak amplitudes of a few tenths of a meter per second. The phase of the semidiurnal cycle in zonal wind is approximately...