Sea-breeze - Cloud Structure In Satellite Images

by FMI and KNMI

A Sea-Breeze is a thermally driven circulation on the coastlines of sea and large lake areas. It is commonly observed during the spring and summer, when the temperature difference between sea and adjacent land areas is large.
The first example below presents a lifecycle of a Sea-Breeze front in 4 successive images over the southwest coast of France and the southeast coast of Spain. In the E-view RGB (combination of HRV + IR10.8) the developing of the convective clouds can be observed. Especially over SW France the track of the Sea-Breeze front inland and the widening of the cloud free area are easy to detect. The convective clouds of the Sea-Breeze front over southern Spain develop at the southeast side of the mountains inland; the decaying at 16.00 UTC is evident.
02 May 2009/09.00 UTC - Meteosat 9 HRV/IR10.8 image
02 May 2009/10.00 UTC - Meteosat 9 HRV/IR 10.8 image
02 May 2009/13.00 UTC - Meteosat 9 HRV/IR 10.8 image
02 May 2009/16.00 UTC - Meteosat 9 HRV/IR 10.8 image
In the VIS image loop below, the development of the Sea-Breeze can be seen as rather rapid growth and spreading of cumulus cloudiness around local noon. During the afternoon the Sea-Breeze develops and a cloud-free area on the west coast of Finland and E. Sweden moves slowly inland.
22 April 2009/14.00 UTC - Meteosat 9 HRV image
09.00 - 15.00 UTC hourly image Loop
The images below are examples of the Airmass RGB, to the left, and the combination of a VIS(0.6), NIR(1.6) and IR(10.8) to the right. All channels, used in the Airmass RGB, are not applicable to the shallow convection in the Sea-Breeze front, unless of course in situations where the Sea Breeze front will act as a first trigger to deep convection, associated with upper air features. This is not the case in this example.
22 April 2009/14.00 UTC - Meteosat 9 WV6.2/WV7.3/IR 9.7/IR 10.8 (Airmass RGB) image
22 April 2009/14.00 UTC - Meteosat 9 0.6/1.6/10.8 image
The image on the right hand side is an example of another RGB - combination. The difference in cloud structure between the convective clouds in the Sea-Breeze front over Normandy, the marine low level clouds over the British Channel and the remnants of low level clouds in the coastal districts southwest of Normandy are hardly to detect. Apparently a combination of 0.6 and 1.6 micrometre is not favourite for detection of this kind of different cloud types, but the superadded IR - channel makes it easy to distinguish the high level clouds more to the east over France.
19 May 2009/11.00 UTC - Meteosat 9 (WV6.2-WV7.3)/(IR9.7-IR10.8)/WV6.2 (Airmass RGB) image
19 May 2009/11.45 UTC - Meteosat 9 HRV image
A second example on the use of Airmass RGB and HRV is presented in the images above. The bluish colour over the south part of the North Sea, The Netherlands and the north part of France clearly indicates the Sea Breeze development is in the same, polar air mass. Over the United Kingdom and The Channel Islands the bluish colour changes into reddish : dry descending stratospheric air above the original polar air. High level clouds appear as white clouds in the Airmass RGB, the lower convective clouds, associated with the Sea Breeze front well depicted over the north west part of France in the HRV - image right, are hardly recognizable. Unfortunately the high level clouds over the west part of The Netherlands make the identification of the Sea Breeze difficult.
19 May 2009/11.00 UTC - Meteosat 9 (WV6.2-WV7.3)/(IR9.7-IR10.8)/WV6.2 (Airmass RGB) image
19 May 2009/11.45 UTC - Meteosat 9 HRV image
The images above show an evolution of a Sea-Breeze front over The Netherlands. More information of this specific situation is available in the next chapters.

Appearance in AVHRR images

AVHRR images help to locate the Sea-Breeze more accurately over land because of the better spatial resolution. Even quite small cumulus clouds can be seen.
The diurnal variation of Sea-Breeze cloudiness and the track of the Sea-Breeze front can be studied by using consecutive AVHRR images.
31 May 2001/14.08 UTC - NOAA RGB image (channel 1, 2 and 4)
31 May 2001/14.08 UTC - NOAA RGB image (channel 3, 4 and 5)
In the images above the Sea-Breeze on the Scandinavian coasts are the cloud-free areas more or less following the shape of coastline. Cumuliform cloudiness marking the Sea-Breeze boundary appear as lumps of white - bluish clouds over land.
In western Finland, along the Gulf of Botnia, the convective clouds of the Sea-Breeze front form a line almost parallel to the coast. The extension of the Sea-Breeze inland, although the RH of the air mass further inland is too low to support any cumulus development, is clear.

Menu Of Sea-breeze
Meteorological Physical Background