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Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood Swedish Institute of Space Physics, Kiruna, Sweden
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Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

Jan 18, 2016

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Page 1: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

Science applications for EISCAT-3D: possibilities for atmospheric research

from the mesosphere down to the troposphere

Evgenia Belova, Sheila KirkwoodSwedish Institute of Space Physics, Kiruna, Sweden

Page 2: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

From mesosphere… PMSE/PMWE research

NLCs. Photo by P.Dalin PMSE with MST 50 MHz and EISCAT VHF radars

Polar Mesosphere Summer Echoes and Noctilucent Clouds, NLCs

Page 3: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

SOFIE – Solar Occultation FOr Ice on the ÀIM satelliteMARA –Moveable Atmospheric Radar for Antarctica

PMSE VR ~ Ne Mice

Now: Ne measurements are not possible during PMSEEISCAT_3D: common volume measurements PMSE from transmitting site and Ne from remote sites

Kirkwood et al., submitted to AnGeo

Page 4: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

Belova et al. 2005

Polar Mesosphere Winter Echoes

Now: strength , spectral widths, vertical winds above ~65 kmEISCAT_3D: horizontal winds, arrival angle (aspect sensitivity), 3D distribution over the whole beamThe same set of parameters as ESRAD but for 60 cm length-scale plus extra.Lower altitudes 50-70 km capabilities to detect more scattering layers

Vhor ~300-400 m/s

Page 5: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

Down to the troposphere…

Novel applications for EISCAT_3D:

• Fine-scale layering in the troposhere/lower stratosphere (up to 12-18 km)

• Turbulent mixing

• Wave propagation in the stratosphere

Scatter of radar wave is on fluctuations of humidity, neutral temperature, Ne

Hocking, 1985

Page 6: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

Fine-scale layers in the troposphere/lower stratosphere

10-19

10-18

10-17

10-16

10-15

6

8

10

12

14

16

1/m

HEIGHT km

16-Jul-2009 00:00

MsqVR ESRAD

10-18

10-17

10-16

10-15

6

8

10

12

14

16

1/m

HEIGHT km

16-Jul-2009 12:00

MsqVR ESRAD

Hooper et al., 2004

July 2009

ESRAD 50 MHz radar

Temperature profiles/structure (both vertical and horizontal)

Page 7: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

Turbulent mixing associated with the tropopause fold:

stratospheric air can be transported into the troposphere

Rao et al. 2006

Page 8: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

GW propagation in the stratosphere

Page 9: Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.

Summary

• Interferometric measurements for mesosphere; 3D-structure

• Lower altitudes coverage with interferometric capabilities; 3D- structure

• Raw data (I&Q) is required

• Extra: Small moveable system (for field/expedition measurements)