Indian Journal of Radio & Space Physics VOLUME 30 NUMBER 4 AUGUST 2001 CONTENTS Strength of equatorial electrojet and geomagnetic activity control on VHF scintillations at the Indian longitudinal zone S Banola , B M Pathan & D R K Rao 163 Comparison of total electron content predicted by IRI with that measured over Ankara Osman Özcan & İbrahim Ünal 172 Short-term ozone trend in India P K Jana , S K Midya & U K De 176 Sodar observed winds in the convective boundary layer at Kharagpur , India, during monsoon 1990 B S Murthy & S S Parasnis Multipath effects on a line-of-sight microwave link S K Sarkar , K Megha Raju , D Punyaseshundu ,M M Gupta , Rajesh Kumar & M V S N Prasad Response of microwave scattering from crop (wheat) and crop covered soil moisture for remote sensing D Singh , S K Sharan & K P Singh Triangular microstrip stacked antenna for dual band operation Prashant Vasistha & Babau R Vishvakarma 181 194 198 205 Notes Ionospheric electron content near anomaly crest as precursor of earthquake M Devi , M K Barman , A K Barbara & A Depueva Characteristics of the observed low latitude very low frequency emission periods and whistler-mode group delays at Jammu Lalmani , Rajou Kumar , Rajesh Singh & Birbal Singh 1 209 214 Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 163-171 Strength of the equatorial electrojet and geomagnetic activity control on VHF scintillations at the Indian longitudinal zone S Banola, B M Pathan & D R K Rao Indian Institute of Geomagnetism, Colaba, Mumbai 400 005 Received 5 April 2000; revised 2 March 2001; accepted 3 April 2001 Amplitude scintillations on 244 MHz radio signals transmitted from geo-stationary satellite, FLEETSAT (73E), were continuously recorded at a network extending from Ujjain (situated north of anomaly crest region) to the equatorial station, Trivandrum, by the Indian Institute of Geomagnetism, Mumbai. Parameters of geomagnetic activity like K-Alibag, Ap and electrojet strength are used to study the association of the amplitude scintillation recordings at the equatorial station, Trivandrum ( dip 1 N ) and at Mumbai ( dip 26 N ), a station south of the anomaly crest region during the high solar activity period 1989-1991. It is observed that an increase in geomagnetic activity (K-Alibag or Ap) suppresses the occurrence of scintillation activity at both the stations, whereas the electrojet strength is found to have no association on the occurrence of scintillations. A total of 77 storms occurring during this period are classified into three types according to Aarons criterion. The time of the maximum intensity of ring current appears to play a role directly or indirectly in establishing the conditions necessary for the equatorial F-layer irregularity generation and inhibition which, in turn, manifests itself in scintillation activity. However, there is about 30-40 % of scintillation activity unaccounted by the magnetospheric electric field alone. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 172-175 Comparison of total electron content predicted by IRI with that measured over Ankara Osman Özcan & Ïbrahim Ünal Department of Physics, Faculty of Arts and Science, Firat University, 23119 Elazig-Turkey Received 30 August 2000; revised 12 January 2001; accepted 20 March 2001 The total electron content (TEC) is a very important parameter for the systems that use transionospheric radio waves. In this paper, TEC measurements obtained with Faraday technique at Ankara (geogr. lat. 40o N, geogr. long. 33o E, geomagn. lat. 36.9o N, dip angle 56.7o) are compared with the TEC obtained by using the International Reference Ionosphere (IRI) model to check the performance of IRI for predicting TEC over this station. The measurements have been taken between October 1975 and June 1976 during low solar activity period. In general, the IRI model was found to give good predictions except for spring equinox and summer solstice time. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 176-180 2 Short-term ozone trend in India P K Jana Department of Chemistry, Howrah Zilla School,Howrah 711 101 and S K Midya Department of Physics, Serampore College, Serampore, Hooghly 712 201 and U K De Environmental Science Program, Jadavpur University, Calcutta 700 032 Received 14 March 2000; Revised received 30 October 2000; accepted 17 April 2001 This paper presents the variation of ozone concentrations at different stations in India and average variation of O3 concentration over India. The results are also compared with those of Halley Bay (76S, 27W), a British Antarctic Survey Station. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 181-193 Sodar observed winds in the convective boundary layer at Kharagpur, India, during monsoon 1990 B S Murthy & S S Parasnis Indian Institute of Tropical Meteorology, Pune 411 008 Received 21 August 2000; revised 17 January 2001; accepted 19 March 2001 Sodar has been installed at Kharagpur (22.2 N, 87.3 E) as a part of the Monsoon Trough Boundary Layer Experiment (MONTBLEX-90) and data were collected during the monsoon period. The monthlymean wind field variation in the convective boundary layer (CBL) at Kharagpur during the S-W monsoon of 1990 has been studied. Monthly-mean horizontal winds were found to be westerly/north-westerly in the convective boundary layer above ~ 600 m in all the monsoon months. In August, mean winds near the surface have become easterly in response to the monsoon depressions formed in the north Bay of Bengal during 15-31 Aug. 1990. Two case studies of depression are studied in terms of winds and thermal structure in the convective boundary layer at Kharagpur. The variation of CBL height over Kharagpur during the onset, active and low/depression phases of the monsoon 1990 is also presented. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 194-197 Multipath effects on a line-of-sight microwave link S K Sarkar1, K Megha Raju2, D Punyaseshundu2, M M Gupta1, Rajesh Kumar1 & M V S N Prasad1 1Radio & Atmospheric Sciences Division, National Physical Laboratory, Dr K. S. Krishnan Road, New Delhi 110 012 2Department of Physics, S K University, Kurnool 518 001 Received 12 May 2000; revised 14 December 2000; accepted 18 April 2001 3 The effects of multipath in relation to the deteriorated performance of a microwave communication link situated between Guntakal and Adoni over the Indian southern region have been investigated. The received signal level under normal condition is usually found to be around 60 dBm. The performance of the link is satisfactory when the signal level is equal to and greater than 74 dBm, which is the satisfactory level of the signal. It has been seen that the link performance starts deteriorating when the signal level reduces to as low as around 75 dBm. The most problematic months during which the performance of the radio link is not up to the satisfactory level are found to be from November to May. The peaks of the disturbances are in the months of February through May. The performance of the link has been found to be disturbed during 2300-0800 hrs LT. On the basis of low signal level (multipath fading), causes of deterioration in relation to meteorological conditions have been determined. In order to counter multipath fading, some techniques have been discussed in this paper. In future this study can also be taken as a reference for designing the microwave communication systems located in the Indian southern region. It is suggested that the link should be equipped with some diversity system. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 198-204 Response of microwave scattering from crop (wheat) and crop covered soil moisture for remote sensing D Singh & S K Sharan Govt. P G Science College, Seepat Road, Bilaspur (CG) 495 006 and K P Singh Department of Electronics Engineering, Banaras Hindu University, Varanasi, (U.P) 221 005 Received 7 February 2000;revised 17 January 2001;accepted 1 March 2001 The present study investigates the potential use of active microwave observations at 9.5 GHz frequency of X-band to monitor soil moisture and vegetation leaf area index (LAI) over a wheat cover for remote sensing. Using an X-band (9.5GHz) scatterometer, measurements have been made out for different growth stage of crop (wheat). The leaf area index (LAI) is an important parameter for understanding the crop characteristics. Here an attempt has been made to highlight the effect of crop (wheat) LAI and crop covered soil moisture (mg) on microwave scattering. Using simple scattering model, an empirical relation has been developed for observing the LAI and mg effect on scattering coefficient. The angular and polarization dependence of scattering coefficient on crop LAI and crop covered soil moisture has been investigated, which indicates that, when incidence angle is less than 30, the crop (wheat) covered soil moisture is well observed, whereas when the incidence angle is greater than 30, crop effect is more dominant at 9.5 GHz. The VV-polarization is more sensitive to sense the crop effect than HHpolarization. This type of study is helpful to make the algorithm for air- or space-borne data to access the crop parameters and crop covered soil moisture. All these data can also be used as reference data for space-borne sensors. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 205-208 Triangular microstrip stacked antenna for dual band operation 4 Prashant Vasistha & Babau R Vishvakarma Department of Electronics Engineering, Institute of Technology, Banaras Hindu University, Varanasi 221 005 Received 31 July 2000; revised received 8 January 2001 Experimental investigations conducted on triangular microstrip stacked antenna (TMSSA) to achieve dual band operation by optimizing the number of elements reveal that TMSSA attains the maximum 10 dB return-loss band of 688.6 MHz for (1+3) structure for second resonance. The air gap spacing of 2.5 mm in (1+1) structure improved 10 dB return-loss (RL) band by 612.14 MHz as compared to 242.3 MHz for zero spacing in first resonance (fr1). It is also observed that 10 dB return-loss band depends heavily on the angular rotation (non-alignment) in the (1+1) structure. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 209-213 Notes Ionospheric electron content near anomaly crest as precursor of earthquake M Devi, M K Barman & A K Barbara Department of Physics, Gauhati University, Guwahati 781 014 and A Depueva IZMIRAN, Troitsk Moscow Region, Russia 142 092 Received 3 November 2000; revised received 28 February 2001 Ionospheric electron content (IEC) values, derived from Faraday rotations of VHF radio beacons from satellites and recorded at an equatorial anomaly crest station, Guwahati (lat.26.2 N, long.91.75E; and situated at a seismically active zone of east Himalayas), have been examined to see if these data could be used as precursor of earthquake. The earthquake events are so selected that the epicentres lie within 12-30 N and 81-120 E. The paper analyses IEC variations during and prior to an earthquake event, in relation to epicentric position. Indian Journal of Radio & Space Physics Vol. 30, August 2001, pp. 214-216 Characteristics of the observed low latitude very low frequency emission periods and whistler-mode group delays at Jammu Lalmani1, Rajou Kumar1, Rajesh Singh2 & Birbal Singh3 1Department of Physics, Engineering College, Srinagar, Camp Jammu, Canal Road, Jammu 180 001 2Atmospheric Research Laboratory, Physics Department, Banaras Hindu University, Varanasi 221 005 3Department of Physics, R .B .S. College, Agra 282 002 Received 29 May 2000; revised 14 September 2000; accepted 28 March 2001 First observations on the relationship between whistlers and periodic very low frequency (VLF) emissions 5 observed at low latitude ground station Jammu (geomagn. lat., 22 26 N; L = 1.17) are presented. The results have been discussed in the present paper. To explain the results it is proposed that the periodic VLF emissions are generated near the equatorial region at L ~ 1.2 as a result of interaction between trapped energetic particles and one-hop whistlers under cyclotron resonance mechanism and propagated to the ground station Jammu in nonducted mode of whistler propagation. 6