Humidity profiles and Arctic Mixed-phase clouds as seen by Airborne W- and G-band radars

07. – 22.02.2024, Kiruna, Sweden

General information

The overarching objective of HAMAG is to test the University of Cologne’s novel G-band radar GRaWAC: G-band Radar for Water vapor and Arctic Clouds aboard AWI’s Polar 6 (C-GHGF) aircraft. GRaWAC will be embedded in a suite of remote sensing instruments (microwave radiometer, lidar, W-band radar) accompanied by dropped atmospheric soundings.

We will take off from Kiruna in Sweden and target mixed-phase clouds over various surfaces (ocean, sea ice in different stages) over the Gulf of Bothnian or along the Atlantic Norwegian coast depending on weather and ice conditions.

And who is we? Enthusiastic cloud scientists from the AWARES group from the Institute for Geophysics and Meteorology at University of Cologne with great support of AWI’s polar aircraft crew.

Follow our flights on flightradar!

Polar-6 took off this morning after a very successful HAMAG campaign.

Today’s research flight was a repetition of RF01 cruising down the Gulf of Bothnia from its northern end down South till we reach the cloud decks that usually form over the open ocean. This year’s ice extension is quite large and it takes us more than one hour to get there. Since the models did not forecast any clouds over the ice in the bay, we planned to use this section for sea ice emissivity measurements. But in contrast to the forecast we could see low clouds covering the ice surface, giving us the chance to see how the new radar performs on these.

Very thin clouds lying on the ground could not be seen, neither by the G- nor by the W-band radar. But very interestingly, the surface return and the patterns of ghost images changed as soon as clouds were in the beam width.

Cruising along the bay we reached thicker clouds organized in several layers. Between the layers, seeder-feeder effects could be seen in the radars as well as DAR signals of up to 7 dB. All in all another very successful flight with a lot of knowledge on our new GRaWAC radar.

We flew over to the Norwegian coast off Tromso to sample beautiful open and closed cell convection (see satellite image) resulting from a cold air outbreak near Svalbard. Crisp and clear flight conditions in Kiruna made take-off and landing smooth, and after passing some textbook lenticularis clouds over the mountain range, we arrived at the very cloudy survey square over the ocean.

With our flight altitude of 10,000ft (about 3.3km), it was harder to distinguish the cells’ structure, but circular, open areas were easy to see in our instruments and with our eyes. Open cells, seen in the upper left corner of the sat image, are circular areas of clear air with clouds forming along the edges: cold air sinks down in the clear air, diverges at surface, and rises at the edges, leading to ring-shaped cloud formation. Closed cells (bottom left) work the other way around: warm, moist air rises in the cell’s center, while cold air sinks around the cell’s edge. The decks here additionally get influenced by air hitting the coast line, leading to accumulation of clouds. Both cell types produce different amount of rain which we could very well observe with both our radars!

Before some of us left the team, we took the chance to take a picture of the HAMAG crew in front of our reliable research platform Polar 6 in Arena Arctica. In the middle underneath the fuselage, you can see the belly pod carrying our two radars, GRaWAC and MiRAC.

Outlook for tomorrow. For the first time, we will try a survey on the Norwegian coast.