---
platform: HALO
flight_id: HALO-20240831a
nickname: Behind the wave
takeoff: "2024-08-31 08:51:01Z"
landing: "2024-08-31 17:41:37Z"
departure_airport: GVAC
arrival_airport: GVAC
crew:
  - name: Silke Groß
    job: PI
  - name: Julia Windmiller
    job: WALES
  - name: Lutz Hirsch
    job: HAMP
  - name: Theresa Mieslinger
    job: Dropsondes
  - name: Sophie Rosenburg
    job: Smart, VELOX, BACARDI
  - name: Anna Volkmer
    job: SpecMACS
  - name: Elina Plesca
    job: Scientist
  - name: Julia Windmiller
    job: Ground contact
instruments:
  BACARDI:
    comment: no entry
    operational: true
  BAHAMAS:
    comment: Some issues
    operational: true
  Dropsondes:
    comment: no entry
    operational: true
  HAMP:
    comment: no entry
    operational: true
  PI-Camera:
    comment: no entry
    operational: true
  Smart:
    comment: None, fully functional
    operational: true
  SpecMACS:
    comment: Fully functional.
    operational: true
  VELOX:
    comment: no entry
    operational: true
  WALES:
    comment: no entry
    operational: true
categories: [ec_under, ec_track, c_north, c_mid, c_south, c_atr]
orphan: true
---

{logo}`PERCUSION`

# {front}`flight_id`

```{badges}
```

## Crew

```{crew-list}
```

## Track

![track](../figures/HALO-20240831a/HALO-20240831a-track.jpeg) 

Flight path superimposed on the natural color image from NOAA's Geostationary Operational Environmental Satellites (GOES) 16 satellite on August 31, 2024 at 15:20 UTC. The location of the aircraft at the time of the satellite image is highlighted.

## Conditions

```{track-animation}
:flight_id: HALO-20240831a
```

Week and narrow ITCZ was observed with extended cirrus layer in the north of the ITCZ

In the northern part of the flight track a Saharan dust layers was detected above marine aerosols, but the dust layer showed less optical thickness than during major Saharan dust events. During the first part of the flight cirrus clouds were at flight level or just above. The southern part of the flight and the southern circle were almost cloud free with thin aerosol layers up to about 5 km altitude. The measurements indicated that those aerosol layers consisted most probably of a mixture of different aerosol types. Some convection was found in the middle layer. Cirrus clouds were present at flight altitude or just below. During the northern circle, cirrus clouds were still present. Below, still dust above marine aerosol could be observed.


## Execution

The flight started almost as planned at 7:50 UTC with a long leg towards the southern point, following the EarthCARE track. At the southern point we turned, returned on track for the southern circle, that could be adapted during the flight to fit the latest forecast. We flew the middle circle as planned, matching perfectly with the convective part of the ITCZ. After flying the northern circle with a small adaption to the latest forecast, we already descended to FL350 to avoid the cirrus clouds at or just below higher flight levels. We met EarthCARE just after the northern exit of the ITCZ in Saharan dust impacted region and continued on the EarthCARE track for a coordinated tandem flight with ATR, guided by King Air. Both aircrafts flew a profile below the HALO flight track to perform in-situ measurement of aerosols and clouds. We turned north of the common flight leg, coordinated again and flew circle around ATR. On the way back to Sal we performed a radar calibration maneuver and landed at 16:40 UTC.

## Impressions

Very narrow ITCZ but extended cirrus cloud cover at or just below flight altitude (FL430). The observed dust layer was less optical thick than during flights before.



````{card-carousel} 2
```{card}
:img-top: ../figures/HALO-20240831a/Flightcrew.jpg
Scientific Crew
```

```{card}
:img-top: ../figures/HALO-20240831a/In_the_north.jpg
In the north
```

```{card}
:img-top: ../figures/HALO-20240831a/Middle_circle_right_window.jpg
Middle circle right window
```

```{card}
:img-top: ../figures/HALO-20240831a/Middle_circle_left_window.jpg
Middle circle left window
```

```{card}
:img-top: ../figures/HALO-20240831a/Down_there_is_METEOR.jpg
Down there is METEOR
```

```{card}
:img-top: ../figures/HALO-20240831a/Match_point_METEOR.jpg
Match point METEOR
```

```{card}
:img-top: ../figures/HALO-20240831a/Perfect_match_ATR.jpg
Perfect match ATR
```


````

## Instrument status & quicklooks

```{instrument-table}
```

````{card-carousel} 2

```{card}
:img-top: ../figures/HALO-20240831a/HALO_20240831a_BACARDI_QL.png
BACARDI
```

```{card}
:img-top: ../figures/HALO-20240831a/20240831_circle_profiles.png

Dropsondes
```

```{card}
:img-top: ../figures/HALO-20240831a/hamp_fullflight_HALO-20240831a.png
HAMP 
```

```{card}
:img-top: ../figures/HALO-20240831a/hamp_ec_under_HALO-20240831a.png
HAMP during EarthCARE underpass
```

```{card}
:img-top: ../figures/HALO-20240831a/hamp_radar_ec_under_HALO-20240831a.png
Radar during EarthCARE underpass
```

```{card}
:img-top: ../figures/HALO-20240831a/HALO_20240831a_SMART_QL.png
SMART Time series of upward and downward spectral irradiadiance, and albedo.
```

```{card}
:img-top: ../figures/HALO-20240831a/QL_VELOX_HALO_20240831a.jpg
VELOX broadband channel with EC underpass
```

```{card}
:img-top: ../figures/HALO-20240831a/HALO_20240831a_KT19_QL.png
KT19 Timeseries of brigthness temperature.
```

```{card}
:img-top: ../figures/HALO-20240831a/HALO-20240831-wales-ec.png
WALES (backscatter, polarization and humidity) at EC overpass
```

```{card}
:img-top: ../figures/HALO-20240831a/0831-wales-3d.jpg

WALES (3D backscatter)
```

```{card}
:img-top: ../figures/HALO-20240831a/0831-wales-x.jpg

WALES (cross section)
```

```{card}
[![specMACS RGB snapshots](../figures/HALO-20240831a/quicklook_20240831_polb_small.png)](https://www.meteorologie.lmu.de/~quicklooks/specMACS/PERCUSION/quicklooks/polcams/quicklook_20240831_polb.png)
specMACS RGB snapshots from polb (lower right) with EarthCARE underpass marked in red. Find further quicklooks [here](https://www.meteorologie.lmu.de/~quicklooks/specMACS/PERCUSION/flight_HALO-0831.html).
```

````
