Abstract. Spatial and temporal variability of the Marine At-mospheric Boundary Layer (MABL) height for the Indian Ocean Experiment (INDOEX) study period are examined us-ing the data collected through Cross-chained LORAN (Long-Range Aid to Navigation) Atmospheric Sounding System (CLASS) launchings during the Northern Hemispheric win-ter monsoon period. This paper reports the results of the analyses of the data collected during the pre-INDOEX (1997) and the INDOEX-First Field Phase (FFP; 1998) in the lati-tude range 14 ◦ N to 20 ◦ S over the Arabian Sea and the Indian Ocean. Mixed layer heights are derived from thermodynamic profiles and they indicated the variability of heights rang-ing from 400 m to 1100 m during daytime depending upon the ...
36-41Upper ocean thermal structure off the coast of Karwar during the withdrawal of monsoon (15 to 3...
The atmospheric boundary layer (ABL) is the lowest layer of the atmosphere where surface effects are...
The thermodynamical structure of the atmospheric boundary layer over the Deccan plateau region has b...
Spatial and temporal variability of the Marine Atmospheric Boundary Layer (MABL) height for the Ind...
This paper describes the results of the measurement of the Marine Boundary Layer (MBL) height from s...
The variability in boundary-layer structure over the Indian Ocean during a north-east monsoon and th...
The characteristic features of the marine boundary layer (MBL) over the Indian Ocean during the nort...
The Indian component of the Intensive Field Phase of Indian Ocean Experiment conducted onboard Ocean...
376-390The characteristic features of the marine boundary layer (MBL) over the Indian Ocean during ...
During the IFP-99 of the INDOEX programme, an Indo-French joint scientific team conducted 17 constan...
The thermodynamic structure of the Atmospheric Boundary Layer (ABL) over the Arabian sea region has ...
In this study an attempt has been made to examine the evolutionary features of the dynamic and therm...
Sea Surface Height (SSH) variability in the Indian Ocean during 1993-1995 is studied using TOPEX/POS...
258-264Influences of wind stress (tau) and wind stress curl (Grad Gamma) on the short term variabili...
This study presents an analysis of observed data sets from multiple sources, including observations ...
36-41Upper ocean thermal structure off the coast of Karwar during the withdrawal of monsoon (15 to 3...
The atmospheric boundary layer (ABL) is the lowest layer of the atmosphere where surface effects are...
The thermodynamical structure of the atmospheric boundary layer over the Deccan plateau region has b...
Spatial and temporal variability of the Marine Atmospheric Boundary Layer (MABL) height for the Ind...
This paper describes the results of the measurement of the Marine Boundary Layer (MBL) height from s...
The variability in boundary-layer structure over the Indian Ocean during a north-east monsoon and th...
The characteristic features of the marine boundary layer (MBL) over the Indian Ocean during the nort...
The Indian component of the Intensive Field Phase of Indian Ocean Experiment conducted onboard Ocean...
376-390The characteristic features of the marine boundary layer (MBL) over the Indian Ocean during ...
During the IFP-99 of the INDOEX programme, an Indo-French joint scientific team conducted 17 constan...
The thermodynamic structure of the Atmospheric Boundary Layer (ABL) over the Arabian sea region has ...
In this study an attempt has been made to examine the evolutionary features of the dynamic and therm...
Sea Surface Height (SSH) variability in the Indian Ocean during 1993-1995 is studied using TOPEX/POS...
258-264Influences of wind stress (tau) and wind stress curl (Grad Gamma) on the short term variabili...
This study presents an analysis of observed data sets from multiple sources, including observations ...
36-41Upper ocean thermal structure off the coast of Karwar during the withdrawal of monsoon (15 to 3...
The atmospheric boundary layer (ABL) is the lowest layer of the atmosphere where surface effects are...
The thermodynamical structure of the atmospheric boundary layer over the Deccan plateau region has b...