Climate change in the D-region

Slides:



Advertisements
Similar presentations
Wot, no interferometer? Milan et al. (1997)
Advertisements

The challenges and problems in measuring energetic electron precipitation into the atmosphere. Mark A. Clilverd British Antarctic Survey, Cambridge, United.
Chapter 3 – Radio Phenomena
1 Effects of solar activity, co-rotating interaction regions, and climate change on thermospheric density during the solar cycle 23/24 minimum Stan Solomon.
Propagation models What are they for? Regulatory vs. scientific issues. Modes of propagation. The models.
BELGRADE DATABASES - ionospheric observations and detections astro- and geophysical phenomena by radio signals Aleksandra Nina Institute of Physics, Belgrade.
Using a DPS as a Coherent Scatter HF Radar Lindsay Magnus Lee-Anne McKinnell Hermanus Magnetic Observatory Hermanus, South Africa.
The Day-Night Terminator Prepared by Morris Cohen and Amanda Angell Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global.
ALTITUDE PROFILES OF ELECTRON DENSITY DURING LEP EVENTS FROM VLF MONITORING OF THE LOWER IONOSPHERE Desanka Šulić 1 and Vladimir Srećković 2 1 Institute.
The Firefly Satellite Mission at Siena Student Participation 12 Undergraduates 3 High-school Students 3 Departments –Physics & Astronomy –Computer Science.
Subionospheric VLF propagation
Damping of Whistler Waves through Mode Conversion to Lower Hybrid Waves in the Ionosphere X. Shao, Bengt Eliasson, A. S. Sharma, K. Papadopoulos, G. Milikh.
VLF measurements of lightning induced electron precipitations and their effects on the D-region electron density profile D. Šulić, and V. D. Šulić 1, and.
Theoretical Study & Modelling of the Intensity Distribution of VLF Signals Tamal Basak [1], Sujay Pal [1], S K Chakrabarti [1,2] 1] S N Bose National Centre.
Targeted VLF Wave-injection Experiments Mark Gołkowski MURI Review Stanford University February 18, 2009.
22 July, 2009 Total Solar Eclipse: Effect on D-region Ionosphere Dynamics as Studied from AWESOME VLF Observations Rajesh Singh B. Veenadhari, A.K. Maurya.
1 Sferics and Tweeks Prepared by Ryan Said and Morris Cohen Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME.
VLF sub-ionospheric signals and Earthquake precursor signatures? Results from the studies of some recent Earthquakes Ajeet K Maurya, Rajesh Singh, B. Veenadhari.
A PRE-STUDY OF AUTOMATIC DETECTION OF LEP EVENTS ON THE VLF SİGNALS.
Characteristics of VLF Tweeks Nedra Tounsi & Hassen Ghalila Laboratoire de Spectroscopie Atomique Moléculaire et Applications 1 In this spectrogram recorded.
AERIALS AND RADIO FREQUENCY PROPAGATION By Farhan Saeed.
Y. Bouderba, S. Naitamor, O. Boumia Research Center on Astronomy, Astrophysics and Geophysics. CRAAG (Algeria). 1 International School of Space Science,
RADAR Detection of Extensive Air Showers Nils Scharf III. Physikalisches Institut A Bad Honnef Nils Scharf III. Physikalisches Institut A Bad.
Lecture 13-15: Transmission media Aliazam Abbasfar.
Signal Propagation Propagation: How the Signal are spreading from the receiver to sender. Transmitted to the Receiver in the spherical shape. sender When.
Importance Of Very Low Frequency Radio Signal Data Registered By VLF-receiver System A. Nina, V. Čadež and V. Srećković Institute of Physics, Belgrade,
CLIMATE CHANGE INDICATORS: UPPER ATMOSPHERE.  Global Temperatures  GHG emissions  Heat waves  Drought  Precipitation  Flooding  Cyclones  Sea.
Radio Propagation Technician License Class Session 3 N1AW revised 4/2013.
Ozone problem Calculate the dependence of O 3 and O with altitude. In class I only showed qualitatively Use an O 2 density of n 2 (z) = n 2 (0)exp[-z/H].
Oct. 23, 2006 Midterm Marked. –Average: 73%. 6 below, 9 above –Answer Key posted: s/nten216/Tests/NTEN216_Midterm1WithAns.
Rory J Gamble1, Craig J Rodger1, Mark A Clilverd2,
Radio Propagation: the key to communication … and its role in clandestine operations during WWII.
Vida Žigman, UNG, Nova Gorica,Slovenia ESWW10 Antwerp, November 2013 Modelling flare induced ionization enhancements of the lower ionosphere with.
Operational and Scientific Results Obtained from AWESOME Receivers in India: Setup under IHY/UNBSSI Program Rajesh Singh, B. Veenadhari, A.K. Maurya, P.
Acoustic wave propagation in the solar subphotosphere S. Shelyag, R. Erdélyi, M.J. Thompson Solar Physics and upper Atmosphere Research Group, Department.
Transient response of the ionosphere to X-ray solar flares Jaroslav Chum (1), Jaroslav Urbář (1), Jann-Yenq Liu (2) (1) Institute of Atmospheric Physics,
Ground-based transmitter signals observed from space: ducted or nonducted? Craig J. Rodger Department of Physics University of Otago Dunedin NEW ZEALAND.
Radio Wave Propagation
Project presentation - Significant parameters for satellite communication.
Thermocline & Pycnocline
Unit 9 Section 2: Solar Energy and the Atmosphere
Shadowing.
British Antarctic Survey
pre-reversal enhancement of the evening vertical plasma drifts
Blocked from the Sun’s Rays: Predicting how the 2017 Total Solar
Chapter 8 Antennas Propagation Dave Piersall, N6ORB.
Visit for more Learning Resources
FACULTY DEVELOPMENT PROGRAMME on EC ANTENNA AND WAVE PROPAGATION
Prediction of fading and link budget in land-satellite (LEO) communication Tal Nir & Ziv Gitelman Department of Communication Systems Engineering , Ben-Gurion.
CEDAR Frontiers: Daytime Optical Aeronomy Duggirala Pallamraju and Supriya Chakrabarti Center for Space Physics, Boston University &
Ionospheric Research Lab
Tropo-Scatter Link Budget
AMATEUR RADIO TRAINING
Atmospheric and ionospheric parameter variations inferred from sub-ionospheric seismo-electromagnetic VLF/LF observations K. Schwingenschuh1, H. U. Eichelberger1,
EASC 11 Chapters 14-18: The Atmosphere
AMATEUR RADIO TRAINING
Refining AWDANet performance: a decade of whistlers
IONOSPHERIC PERTURBATIONS INDUCED BY SOLAR X-RAY FLARES
Introduction to Atmospheric Science at Arecibo Observatory
Study of the sporadic E (Es) layer by GPS radio occultation (RO)
The Atmosphere Layers and aerosols.
Charles Lin1, Jia-Ting Lin1, Loren Chang2, Yang-Yi Sun2
Chelmsford Amateur Radio Society Intermediate Course (6) Propagation
OC3570 Operational Meteorology
Effects and magnitudes of some specific errors
Chelmsford Amateur Radio Society Intermediate Course (6) Propagation
Course: Topics in Discharge Phenomena
Challenges of Radio Occultation Data Processing
The Ionosphere Equatorial Anomaly.
The Vertical Structure of the Martian Ionosphere
Presentation transcript:

Climate change in the D-region Mark A. Clilverd1, Roger Duthie1, Craig J. Rodger2, Rachael L. Hardman1,4, and Keith H. Yearby3 1British Antarctic Survey (NERC), Cambridge, UK. 2Department of Physics, University of Otago, Dunedin, New Zealand. 3Department of Control Engineering, University of Sheffield, Sheffield, UK. 4Now at School of Mathematics and Statistics, University of Sheffield, Sheffield, UK. STP14: Session 3.2 - Long term variability of the whole atmosphere Toronto, Wednesday, 11th July 2018

The expected effect of greenhouse gas increases. Laštovička et al., Ann. Geophys. 2008. Trends in the [lower] ionosphere below 100 km, derived from LF radio propagation data, have been studied primarily in Europe. Trends in the lowermost part of the ionosphere could be investigated with the use of the VLF radio wave propagation measurements over long distances. As far as we know, such an analysis has not yet been made. A very important point to be discussed in relation to long-term trend studies is the various uncertainties in data and also the long-term non-stability of measurements.

What experiment stays the same for 40+ years? The NAA VLF transmitter 1MW output, since 1961 (~20 MW input). 24.0 kHz since 1983. 17.8 kHz before that.

Making measurements of VLF radio waves: Radio transmissions at Very Low Frequencies (VLF) largely trapped between the conducting ground (or sea) and the lower part of the ionosphere (70-90 km) , forming the Earth-ionosphere waveguide. Changes in the ionosphere cause changes in the received signal. The nighttime D-region is primarily generated by the ionisation of NO by solar Lyman-α (121.6 nm) scattered by the neutral hydrogen in the Earth’s geo-corona.

DEMETER view of NWC at 19.8 kHz From: J.-A. Sauvaud et al., Geophys. Res. Lett., 35, L09101, doi:10.1029/2008GL033194, 2008. ‘provides a nice example of diffraction pattern’

Halley, VLF receiver operating since 1971

NAA at Halley: detecting the minima Night Sunrise modal minima Day 1971-1975: Paper charts on a multi-channel receiver NAA trace Time (UT)

LWPC amplitude versus distance Previous work on sunrise modal minima times (Clilverd et al., Radio Sci., 34(4), 939-948, 1999) LWPC amplitude versus distance Variation of NAA modal minima over a year Measured just under the ionosphere Sunrise at a receiver at 75km altitude. Measured near ground level

Changing Frequency [NAA was 17.8 kHz in 1971, but changed to 24.0 kHz in 1983 staying the same since.] Changing frequency changes the locations of the nighttime modal minima. But we can model the change. NAA, 24.0 kHz NAA, 17.8 kHz

The timing of sunrise at the Tx in Nov/Dec, and fringe distance from Tx 10:43:40 UT on 28 November. Equivalent to the terminator crossing overhead of the transmitter at an altitude of 71.5km +/- 2km (i.e., +/- 30 s) LWPC was used to investigate the sensitivity of the NAA nighttime fringe distance to Wait’s electron density profile parameters: h′ and β. It was found that the NAA fringe distance was relatively insensitive to β, but a contraction of 10% could be achieved through a reduction in nighttime h′ by 3 km. Both sunspot activity samples show gradients of ~5 km/year, i.e., 10% change in fringe distance in 45 years.

Summary Using a VLF transmitter in the same location, same power, we have investigated where modal minima occur on the great circle path to Halley over 40+ years. The transmitter fringe pattern at 70-80 km altitude (lower D-region) appears to be contracting at a rate of 4-6 km/year. The 10% fringe pattern contraction is consistent with a height change in the nighttime D-region of ~3 km (downwards). At a fixed altitude electron density would increase. This is consistent with the predicted effects of greenhouse cooling /contraction of the mesosphere. Reference: Clilverd, M. A., R. Duthie, C. J. Rodger, R. L. Hardman, and K. Yearby, Long-term climate change in the D-region, Nature: Scientific Reports, 7:16683, doi:10.1038/s41598-017-16891-4, 2017.

Uncertainties 2012: We use 10 s averages, timing <1 second 1971: 0.5 mm or ~30 seconds, time accurate to within 30 secs. Path length 13,000 km – 4 hours for terminator to sweep along path – ~50 km/min Movement of modal feature is ~70 km/1 km in H prime. Timing uncertainties are therefore about 25km, which is ~0.3 km in H prime. Halley Nov 2015 modal min times are unstructured, and need further investigation.