Observing the life cycle of a storm

 

Instruments on board Meteosat Third Generation satellites enable meteorologists to better monitor severe storms

Instruments on board the Meteosat-12 and Meteosat Third Generation Sounder 1 satellites provide complementary observations that can be used to better forecast and monitor storms even before the first clouds have developed.

Last Updated

23 June 2025

Published on

23 June 2025

Life-threatening thunderstorms can form fast.

In a matter of just a few hours, clear skies can give way to lightning, hail, and severe winds. Making it possible to better monitor the complete life cycle of a storm – from before any signs are even visible to a mature storm – has the potential to save lives.

A first for Europe

Set to be launched this July, the Meteosat Third Generation Sounder 1 (MTG-S1) satellite will make a crucial contribution to doing just that. The first European satellite in geostationary orbit to carry a hyperspectral sounder, its instruments will complement those of the first satellite in the MTG fleet, Meteosat-12.

Once in orbit, these two MTG satellites will follow the Earth as it rotates, remaining in their shared orbital slot about 36,000km above where the equator cuts through the Gulf of Guinea, off the west coast of Africa. By sharing an orbital slot – a technique known as colocation – the observations collected by the instruments on each platform will be as though from the same platform. Together, these instruments will provide data that will enable meteorologists to level up their forecasting of severe storms.

“Before MTG, some part of the picture of the development of a storm was missing,” said Dr Jochen Grandell, EUMETSAT’s MTG Programme Scientist.

“For example, we saw the growing clouds, however, we did not see the early lightning, which indicates a storm’s severity. Now, meteorologists will be able to receive observations for the whole life cycle of a storm using data from MTG instruments together.”

The initiation of severe thunderstorms hinges on atmospheric instability – an overlap of low-level humidity and strongly decreasing temperature with increasing height – combined with lift caused by a convergent wind field or mountain range.

“As of now, this developing instability cannot be followed by measurement data,” said Alois Holzer, Director of Operations at the European Severe Storm Laboratory.

Collocated observations from the Infrared Sounder, the Flexible Combined Imager, and the Lightning Imager on MTG satellites can be used by meteorologists to more accurately predict severe storms further in advance

“Currently, the only way of observing the Earth’s atmosphere in certain regions is by using in-situ instruments such as weather balloons and probes attached to aircrafts – without them, there is simply no way of observing what is happening above the surface. Forecasters can rely on models for guidance but cannot follow the conditions with measured data to see if things are developing as expected. That is what is so exciting about the new sounder satellite – for the first time, it will be possible to closely follow how the atmosphere prepares itself for a thunderstorm.”

The 4D weather cube, depicted in the animation below, is a valuable tool for visualising the complementarity of four different data sets – atmospheric profiles, winds, convection, and lightning – from three key MTG instruments.

Monitoring the life cycle of a storm

Complementary observations will make this possible by measuring a storm at different stages of its formation. Before the first clouds have formed, the Infrared Sounder on board MTG-S1 will provide temperature and water vapour profiles, measurements of temperature and humidity at different altitudes every 30 minutes for Europe, and with less frequency over Africa and the surrounding regions.

“Before the initiation of a storm takes place, a forecaster can use observations from the Infrared Sounder to see if the moisture in the atmosphere is increasing and if the temperature profile is steepening, which means that the temperature is decreasing by height more quickly,” said Holzer.

“This indicates that unstable conditions are developing. Observations from the Infrared Sounder will enable meteorologists to follow these changes. Seeing these before clouds have formed is really a game changer in terms of lead time.”

Next in the development of a storm comes the valuable contribution of the Flexible Combined Imager on board Meteosat-12. By providing images of the entire Earth disc every ten minutes, this instrument enables meteorologists to better track winds and convection, the vertical movement of heat and moisture through the atmosphere.

Using data from the Flexible Combined Imager, meteorologists will also be able to detect temperature differences at the tops of clouds, which is crucial for identifying the conditions that lead to storm intensification – high and cold cloud tops are an indicator of severe convection.

Storm Hans over Scandinavia as observed by the Flexible Combined Imager on board Meteosat-12 on 7 August 2023
 A storm over Western Europe as detected by the Lightning Imager on Meteosat-12 11-12 July 2023

Lastly, once a storm has developed, observing lighting flashes is essential for keeping people safe. Another Meteosat-12 instrument, the Lightning Imager, measures total lightning flashes including those within and between clouds, as well as from clouds to the ground, across Europe, Africa, and the surrounding regions.

“The Lightning Imager makes it possible to see the early lightning, which often comes in an early phase of convection before you have very strong winds and precipitation, including hail,” said Grandell.

“Lightning typically starts as small intracloud lightning, which is inside the cloud and is not something you might be able to observe very easily without this instrument. Then comes the first cloud-to-ground lightning, which is definitely visible. But you already have severe weather at that point, so if you only start observing lightning then, it is a bit late.

“The benefit of the Lightning Imager is being able to start detecting lighting early. With this lead time, you can observe the lightning jump, which is when the rate of lightning strikes increases rapidly. This indicates that a storm is becoming severe.”

Keeping people safe

More accurately forecasting storms further in advance benefits people in a wide range of situations.

“There are all kinds of applications where people need this information fast,” said Holzer.

“For example, if there is a children’s sailing competition on a lake or at a seashore, what does it mean when there is a big thunderstorm approaching this area? All those children will need to be brought to land. Also, storms could endanger people hiking in the mountains or cause the very quick discharge of a river in a heavily populated area that would flood underground garages.

“MTG instruments play a role in increasing the lead time for meteorologists to forecast storms and issue severe weather warnings. Every piece that we can add to complete this picture of forecasting storms helps.”

Author:

Sarah Puschmann