Abstract
During a two-year period measurements were obtained along four meteorological masts placed from the coastline to 30 km inland at the North Sea coast of Jutland in Denmark (the JYLEX experiment). The data were organized to show the behaviour of the most important parameters of the turbulent structure when a flow passes from over-sea to over-land conditions. The results are stratified according to season, day and night, and wind direction. (au) (4 tabs., 14 ills., 12 refs.).
Citation Formats
Sempreviva, A M, Larsen, S E, and Mortensen, N G.
Experimental study of flow modification inland from a coast for nonneutral conditions.
Denmark: N. p.,
1992.
Web.
Sempreviva, A M, Larsen, S E, & Mortensen, N G.
Experimental study of flow modification inland from a coast for nonneutral conditions.
Denmark.
Sempreviva, A M, Larsen, S E, and Mortensen, N G.
1992.
"Experimental study of flow modification inland from a coast for nonneutral conditions."
Denmark.
@misc{etde_10144618,
title = {Experimental study of flow modification inland from a coast for nonneutral conditions}
author = {Sempreviva, A M, Larsen, S E, and Mortensen, N G}
abstractNote = {During a two-year period measurements were obtained along four meteorological masts placed from the coastline to 30 km inland at the North Sea coast of Jutland in Denmark (the JYLEX experiment). The data were organized to show the behaviour of the most important parameters of the turbulent structure when a flow passes from over-sea to over-land conditions. The results are stratified according to season, day and night, and wind direction. (au) (4 tabs., 14 ills., 12 refs.).}
place = {Denmark}
year = {1992}
month = {Jan}
}
title = {Experimental study of flow modification inland from a coast for nonneutral conditions}
author = {Sempreviva, A M, Larsen, S E, and Mortensen, N G}
abstractNote = {During a two-year period measurements were obtained along four meteorological masts placed from the coastline to 30 km inland at the North Sea coast of Jutland in Denmark (the JYLEX experiment). The data were organized to show the behaviour of the most important parameters of the turbulent structure when a flow passes from over-sea to over-land conditions. The results are stratified according to season, day and night, and wind direction. (au) (4 tabs., 14 ills., 12 refs.).}
place = {Denmark}
year = {1992}
month = {Jan}
}