SYNOPTIC METEOROLOGY

All Items

• Fourier expansion techniques in objective analysis

  Y. RAMANATHAN, D. R. SIKKA

  145-152

• Formation, intensification and unusual movement of the storm of 8 November 1965

  DR SWAMINATHAN

  197-205

• FORMATION OF TROPICAL CYCLONES IN THE BAY OF BENGAL

  G. S. GANESAN , A. MUTHUCHAMI , E. R. SUKUMAR

  235-242

• Forecastmg storm ramfall over Bhagirathi catchment due to depressions/cyclonic storms

  G. R. GUPTA, K. K. SRIVASTAVA, H. A. MEHRA , T. A. JASRA

  139-156

• Forecasting models of daily maximum and minimum temperature – A comparative study for Dumdum airport

  K. SEETHARAM

  609-616

• Forecasting maximum and minimum temperature over airports with special relevance to aviation in flight planning

  R. SURESH

  121-128

• Fluctuations of monsoon activity

  GEORGE ALEXANDER, R. N. KESHAVAMURTY, U.S. DE, R. CHELLAPPA, S. K. DAS, P. V. PILLAI

  76-87

• Extreme wind speeds over India

  P. S. HARIHARAAYYAR , S. C. GOYAL

  67-70

• Existence of low level westerly Jet Stream over peninsular India during July

  P. V. JOSEPH, P. L. RAMAN

  407-410

• EXCEPTIONALLY HEAVY RAINS IN AND AROUND PATNA CITY IN SEPTEMBER 1967 : A CASE STUDY OF ID-TROPOSPHERIC INTERACTION BETWEEN AN EASTERLY WAVE AD A WESTERLY WAVE

  S. SEN GUPTA

  599-600

• Exceptional rainfall event of 26th July, 2005 over Mumbai - Analysis of radar echoes and rainfall

  RAJENDRA KUMAR JENAMANI , S. C. BHAN

  366-376

• Evolution of two troughs in the tropical Indian Ocean and their characteristic features

  M.S. SINGH, B. Lakshmanaswamy

  395-398

• Evaluation of the use of satellite photography in determining the location and intensity changes of tropical cyclones in the Arabian Sea and the Bay of Bengal

  D. R. SIKKA

  305-312

• Energetics of the lower tropospheric eddies in wave number domain during northern summer monsoon

  S. M. BAWISKAR, M. D. CHIPADE, S. S. SINGH

  119-126

• Effects of off-shore vortices on rainfall along the west coast of India

  P.A. GEORGE

  225-240

• EFFECT OF WESTWARD MOVING CLOUD ORGANISATIONS IN WEST AND NEAR EQUATORIAL PACIFIC OCEAN ON THE MONSOON RAINFALL OF INDIA

  ASOI LAL , R. S. SUNDAR

  315-324

• Effect of smoothing initial height field on vertical motion

  U.S. SINGH , H. S. RATHOR

  146

• Effect of monsoon depression of east coast at some distant region in west

  ASOI LAL , R. S. SUNDAR

  453-460

• Effect of High Level Divergence on the Rainfall Distribution over northwest India associated with a southwest monsoon depression

  K. S. VENKATARAMAN, N. S. BHASKARA RAO

  411-420

• Effect of eastward moving cloud clusters over northwest India and neighbourhood on the Indian summer monsoon

  ASOI LAL, R. S. SUNDER , S. P. JOSHI

  25-30

• Dynamics of thunderstorms

  S. Mull, Y.P. RAO

  116-136

• DOES BREAK MONSOON ALWAYS MEAN SUBDUED RAINFALL OVER INDIA? - AN ANALYSIS OF ROLE OF OFF-SHORE TROUGH IN THIS ASPECT

  RAJENDRA KUMAR JENAMANI

  572-579

• Diurnal Magnetic variation in Equatorial Regions

  S. K. PRAMANIK, S. YEGNA NARAYANAN

  212-216

• Distribution of precipitable water contents over Indian monsoon region

  VR DURAI, SKROY BHOWMIK, HR HATWAR

  241-250

• Distribution of mean monthly surface/upper air parameters during July-August months of 1982-83 and 1987- 88

  K. SEETHARAM

  255-270

• Distinct synoptic patterns associated with pre-break onset phase and revival of normal monsoon phase

  JENAMANI RAJENDRA KUMAR

  591-598

• Distant effects of monsoon depressions on weather over west Rajasthan

  A. K. MUKHERJEE , B. SHYAMALA

  47-53

• Discussion of some sounding data over the eastern Indian Ocean and central Arabian Sea during 1976 monsoon period

  S. K. SUBRAMANIAN

  135-137

• DISASTROUS WEATHER EVENTS OF EXTREME HEAVY RAINFALL IN WEST BENGAL

  P. G. GORE, P. R. JOSHI, S. K. DIKSHIT

  513-517

• Development of monsoon breaks due to heat source over northwest India

  U. V. BHIDE, P. V. PURANIK, V. R. MUJUMDAR, A. A. KULKARNI, R. H. KRIPALANI

  377-384

• Development of a weather control indication chart Development of a weather control indication chart

  H. SCHULZE-NEUHOFF

  517-522

• Derivation of cloud top heights using HRIR data

  N.S. BHASKARA RAO , V. P. SAXENA

  447-458

• Decaying nature of super cyclone of Orissa after landfall

  S. R. KALSI, S. D. KOTAL, S. K. ROY BHOWMIK

  393-396

• Decaying characteristics of severe cyclonic storms after landfall over east coast of India

  CHARAN SINGH, B. K. BANDYOPADHYAY

  395-400

• DECADAL VARIATIONS IN TRANSLATIONAL SPEED OF CYCLONIC DISTURBANCES OVER NORTH INDIAN OCEAN

  B. GEETHA, S. BALACHANDRAN

  115-118

• Daily summer monsoon rainfall over northeast India due to synoptic scale systems

  M. MOHAPATRA, H. R. BISWAS, G. K. SAWAISARJE

  35-50

• Cyclonic and anticyclonic circulations of 850 hPa over India and adjoining areas based on highly packed hand drawn streamline charts : part 1 - characteristics

  Anish Kumar M Nair, K. V. Sambhu Namboodiri, Mahesh C., Dileep P. K.

  553-568

• Cyclone movement

  A. GEORGE , M. A. SHARMA

  109-116

• Cross-equatorial flow over southeast Asia during the Northeast monsoon

  JOO TICK LIM , LEONG CHUAN QUAH

  5-15

• Convective activity associated with Jet Stream

  D. R. SWAMINATHAN

  247-250

• Contrasting pre-monsoon features associated with early and late onset of southwest monsoon over Kerala

  D. R. PATTANAIK, N. JAYANTHI, A. B. MAZUMDAR

  617-626

• Computation of vertical velocity incorporating release of latent heat of condensation

  K. V. RAO , S. RAJ AMANI

  369-374

• Computation of Streamlines associated with a low latitude Cyclone

  A. C. TANGRI

  401-406

• Comparison of Geostrophic Winds on constant pressure surfaces with observed winds in India

  V. VITTAL SARMA

  41-47

• Clouding over the Arabian Sea and the synoptic situation over India during monsoon

  A. K. MUKHERJEE, G. GURUNADHAM, K. P. PADMANABHAM

  118-124

• Characteristics of natural wind - Pt. II: Turbulent flow

  V. KR. SHARAN

  11-28

• Characteristics of natural wind - Pt. I: Mean flow

  V. KR. SHARAN

  1-10

• CAUSES OF LESS RAIN OVER THE KIRTHAR RANGE THAN OVER THE DECCAN PLATEAU IN THE RAIN SHADOW OF THE WESTERN GHATS AND OF NEAR DESERT CONDITIONS IN THE NORTHWEST OF THE SUBCONTINENT

  YP Rao, BN Desai

  127-128

• CAPE - A link amid thermodynamics and microphysics for the occurrence of severe thunderstorms

  SUTAPA CHAUDHURI , SUCHANDRA AICH BHOWMICK

  249-254

• Bhartiya upmandalon mein 1987 ke dauran madhyam evam bheeshm sukha ke kshetriya vistar ka vargikaran

  Hari Singh, Rajendera Prasad

  841-850