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Remote sensing for resources development and environmental management (Volume 2)

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CC BY: Attribution 4.0 International. You can find more information here.

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fullscreen: Remote sensing for resources development and environmental management (Volume 2)

Multivolume work

Persistent identifier:
856342815
Title:
Remote sensing for resources development and environmental management
Sub title:
proceedings of the 7th international Symposium, Enschede, 25 - 29 August 1986
Year of publication:
1986
Place of publication:
Rotterdam
Boston
Publisher of the original:
A. A. Balkema
Identifier (digital):
856342815
Language:
English
Additional Notes:
Volume 1-3 erschienen von 1986-1988
Editor:
Damen, M. C. J.
Document type:
Multivolume work

Volume

Persistent identifier:
856641294
Title:
Remote sensing for resources development and environmental management
Sub title:
proceedings of the 7th international Symposium, Enschede, 25 - 29 August 1986
Scope:
IX Seiten, Seiten 551-956
Year of publication:
1986
Place of publication:
Rotterdam
Boston
Publisher of the original:
A,. A. Balkema
Identifier (digital):
856641294
Illustration:
Illustrationen, Diagramme
Signature of the source:
ZS 312(26,7,2)
Language:
English
Usage licence:
Attribution 4.0 International (CC BY 4.0)
Editor:
Damen, M. C. J.
Editor:
International Society for Photogrammetry and Remote Sensing, Commission of Photographic and Remote Sensing Data
Publisher of the digital copy:
Technische Informationsbibliothek Hannover
Place of publication of the digital copy:
Hannover
Year of publication of the original:
2016
Document type:
Volume
Collection:
Earth sciences

Chapter

Title:
6 Hydrology: Surface water, oceanography, coastal zone, ice and snow. Chairman: K. A. Ulbricht, Co-chairman: Mikio Takagi, Liaison: R. Spanhoff
Write comment:
Wegen zu enger Bindung kommt es teilweise im Original zu Textverlust.
Document type:
Multivolume work
Structure type:
Chapter

Chapter

Title:
Satellite remote sensing of the coastal environment of Bombay. V. Subramanyan
Document type:
Multivolume work
Structure type:
Chapter

Contents

Table of contents

  • Remote sensing for resources development and environmental management
  • Remote sensing for resources development and environmental management (Volume 2)
  • Cover
  • Title page
  • Title page
  • Title page
  • Table of contents
  • 5 Non-renewable resources: Geology, geomorphology and engineering projects. Chairman: J. V. Taranik, Liaison: B. N. Koopmans
  • 6 Hydrology: Surface water, oceanography, coastal zone, ice and snow. Chairman: K. A. Ulbricht, Co-chairman: Mikio Takagi, Liaison: R. Spanhoff
  • A methodology for integrating satellite imagery and field observations for hydrological régionalisation in Alpine catchments. R. Allewijn
  • The JRC program for marine coastal monitoring. J. A. Bekkering
  • Shape and variability of the absorption spectrum of aquatic humus. H. Buiteveld & F. de Jong, R. Spanhoff, M. Donze
  • Rainlog and preslog: Novel tools for in-situ measurements. D. de Hoop
  • Simple classifiers of satellite data for hydrologic modelling. R. S.Drayton, T. R. E. Chidley & W. C. Collins
  • The delineation and classification of inland wetlands utilizing fcir stereo imagery. Stephen A. Estrin
  • A hydrological comparison of Landsat TM, Landsat MSS and black & white aerial photography. M. J. France & P. D. Hedges
  • Application of remote sensing in hydromorphology for third world development: A resource development study in parts of Haryana (India). A. S. Jadhav
  • Remote sensing of flow characteristics of the strait of Öresund. L. Jönsson
  • Present state, changes and quality of Sologne and Brenne, two French large wetlands, studied with the MSS and TM Landsat data. Michel Lenco, Jean-Pierre Dedieu
  • The quantification of floodplain inundation by the use of LANDSAT and Metric Camera information, Belize, Central America. S. T. Miller
  • Remote sensing as a tool for assessing environmental effects of hydroelectric development in a remote river basin. W. Murray Paterson & Stewart K. Sears
  • Environmental assessment for large scale civil engineering projects with data of DTM and remote sensing. Taichi Oshima & Atsushi Rikimaru, Youichi Kato & Masaharu Nakamura
  • Sea surface temperature studies in Norwegian coastal areas using AVHRR- and TM thermal infrared data. J. P. Pedersen
  • Satellite data in aquatic area research: Some ideas for future studies. Jouko T. Raitala
  • Analysis of Landsat multispectral-multitemporal images for geologic-lithologic map of the Bangladesh Delta. A. Sesören
  • Water quality monitoring of Lake Balaton using LANDSAT MSS data. H. Shimoda, M. Etaya & T. Sakata, L. Goda & K. Stelczer
  • Determination of spectral signatures of natural water by optical airborne and shipbome instruments. D. Spitzer & M. R. Wernand
  • Classification of bottom composition and bathymetry of shallow waters by passive remote sensing. D. Spitzer & R. W. J. Dirks
  • Satellite remote sensing of the coastal environment of Bombay. V. Subramanyan
  • A study with NOAA-7 AVHRR-imagery in monitoring ephemeral streams in the lower catchment area of the Tana River, Kenya. J. W. van den Brink
  • A simple atmospheric correction algorithm for Landsat Thematic Mapper satellite images. P. I. G. M. Vanouplines
  • 7 Human settlements: Urban surveys, human settlement analysis and archaeology. Chairman: W. G. Collins, Co-chairman: B. C. Forster, Liaison: P. Hofstee
  • 8 Geo-information systems. Chairman: J. J. Nossin
  • Cover

Full text

Symposium on Remote Sensing tor Resources Development and Environmental Management / Enschede / August 1986 
779 
Satellite remote sensing of the coastal environment of Bombay 
V.Subramanyan 
Indian Institute of Technology, Bombay 
ABSTRACT: Remote sensing of the coastal environment of Bombay using the Landsat imagery 
(black and white and false-colour paper prints) makes it possible to trace the development 
and evolution of the coast. The coast is indented by many bays, promontories, creeks, tidal 
mudflats, stacks and beaches. It is thus one of rétrogradation. All the creeks follow 
lineaments and there is a triple junction of such lineaments to the east of Bombay. These 
clearly indicate the erosional development of the region by fluvio-marine processes. A 
reconstruction of the initial configuration of the Bombay region is attempted. Marshes, 
raised beaches and littoral concrete point to the emergence of the region in the past. 
The bays and headlands will be eliminated towards the end of the current marine cycle and 
the coast, straightened. Three rows of cuestas of volcanic rocks trending NNE-SSW with 
westerly dipslopes traverse the island lengthwise; there are three aligned lakes. 
1 INTRODUCTION 
The Bombay coast, including that of the 
Salsette island to the north, forms a part 
of the Konkan Coast of the West Coast phy 
siographic division (National Atlas 1964)** 
The geomorphic environment of this coastal 
tract and the neighbouring Nhava-Sheva-Uran 
shoreline to the east was studied using the 
following data products of the Landsat: 
black and white paper print on MSS band 6 
on the scale of 1:250,000 and false-colour 
composite paper print on MSS bands 4 (yel 
low) , 5 (pink) and 7 (blue) on the scale 
of 1:500,000. The images were further mag 
nified during the visual interpretation. 
Geological and geomorphological field 
traverses were undertaken in selected loca 
lities for the collection of ground truth. 
The topographical maps on the scale of 1: 
63360 and the Town Guide Map of Bombay on 
the scale of 1:25,000 were also consulted 
for supplementary data. 
2 SATELLITE DATA 
The black and white image brings out clear 
ly the configuration of the Bombay-Salsette 
coast and the Nhava-Sheva-Uran coast to the 
east. Three well-developed bays, namely, 
the Manori bay, the Mahim bay and the Back- 
bay and the broad embayment between Versova 
and Juhu show up along with their corres 
ponding promontories (Fig.1). Sandy beaches 
can be readily recognised by the white tone 
around Manori, Versova, Juhu, Bandra and 
Girgaon. Rocky beaches with boulders, cobb 
les and gravels as well as wave-cut plat 
forms can be identified at other places 
along the coast by the pale grey tone. The 
cuestas bordering the three lakes and con 
tinuing farther north display a light and 
shade effect on their escarpments and dip- 
slopes. The morphological signature of the 
cuestas south of the Powai lake is a faint 
grey line whereas in the Kanheri Hills in 
the northern part of the island, the cues 
tas occupy a considerable area - about 25 
sq. km. The big c uesta at the centre of the 
Figure 1. A Landsat view of the 
Bombay-Salsette island and the 
neighbouring country to the east 
and southeast on MSS hand 6. The 
coastal and inland features show 
up very well. 
Trombay island in the east also shows up as 
a thick grey line. The mudflats that have 
formed in the tidal zone between the low 
and the high tides are readily recognised 
by their dark grey tone and their locations 
around the creeks. The lakes and the creeks 
appear black whereas the marshes in the 
Mahim and Chembur areas appear as medium 
grey patches. 
The basalts are seen as pale grey areas 
in the Bombay island while the trachytes, 
rhyolites and tuffs in the Salsette island 
appear much paler. The salt fields have 
registered themselves as white streaks, ex 
pectedly. The urban, suburban and vegetated 
areas show a light grey tone. 
The false-colour composite facilitates the
	        

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