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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.

Bibliographic data

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

780 
recognition of all the features described 
above. Tne Sandy beaches show up as white 
strips, the tidal mudflats appear mixed 
areas of pink and blue and the lakes have 
recorded a deep blackksh blue shade. The 
marshes and the swamps are seen as blue are 
as. The basaltic cuestas show a paler shade 
of blue on the escarpments and a darker sha 
de of blue on the dipslopes. The ridge Cre 
stline of the Vikhroli-Ghatkopar range shows 
up as a fine line whereas the Kanheri range 
is seen as a very wide dark pink patch. The 
urban and suburban areea appear as very li 
ght areas with patches of pink representing 
vegetated hills. Open green turfs like the 
race course are seen as deep pink areas. 
The rocky beaches in the Juhu-Bandra stret 
ch show up as wavy blue lines along the sho 
reline. The salt fields are recognised by 
their white tone and the sandy spit at Ver- 
sova is clearly picked up as a fine, white 
projection into the sea. 
3 MAP DATA 
The topographical maps or. the scale of 1: 
63360 and the Town Guide Map on the scale 
of 1:25,000 wexe studied and these have 
added more local details while generally 
confirming the interpretation of the image 
ry. Rocky beaches can be clearly distingui 
shed from sandy beaches. The topographical 
contours not only give an idea about the 
relief dnd slopes but also indicate the 
attitude of the volcanic rocks through the 
landforms which are all structural landfor- 
ms. The tidal range is very clearly under 
stood from the maps and the drainage details 
over the mudflats are exceedingly clear. 
4 FIELD DATA 
Field traverses for the collection of grou 
nd truth have provided data on the rock ty 
pes and their attitudes. Three low ranges 
of volcanic rocks trending NNE-SSW traverse 
the island producing promontories bordered 
by cliffs. The volcanics, dominantly basalts, 
strike NNE-SSW and have westerly dips rang 
ing from 11° to 23°. Trachytes and rhyolites 
are exposed in the Madh island and north 
ward. Tuffs are found in the Kanheri range 
along with agglomerate. Intertrappean sedi 
mentarles are exposed at a number of loca 
lities like Jogeshwari. Dykes of dolerites 
are met with in Trombay and in the Powai 
hills o 
Geomorphological field investigations alo- 
^ the coast over the past ten years have 
revealed the recurrence of accentuated ma 
rine erosion in the area south of Versova. 
No other stretch along the coast has been 
or is undergoing erosion. Shetti and Subra- 
manyan (1985) have studied the spit which 
is trending southwestward from the mouth of 
the Malad creek and have attempted to simu 
late its growth through a computer progra 
mme. 
Field studies also indicate that the mul 
tistorey buildings have given rise to the 
densest concrete jungle in the Back Bay 
area in the southernmost part of the island 
and that urbanization is proceeding at a 
fast pace all along the coast in particular. 
Figure 2. Map showing the lineaments in the 
Bombay region and neighbourhood which appear 
to have controlled the creeks and the river. 
Figure 3. A geomorphic map 
of the Bombay region showing 
sandy beaches (1), rocky bea 
ches (2), marshes (3), tidal 
mudflats (4) and cuestas (5). 
5 DISCUS 
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promontc 
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shown or 
the Thar 
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formed e 
southerr 
trending 
opened c 
region, 
led the 
island e 
area in 
the line 
triple ■ 
region e 
erosion. 
A reti 
had set 
ted the 
highly i 
* ria' ty 
med in 1 
and the 
urbanize 
sional £ 
and thej 
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is takir 
thmic re 
partly ; 
Madh prc 
ing the 
st whiclr 
former, 
the nori 
from ere 
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Versova 
up the t 
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point oi 
stretch 
require; 
by Shet-t 
It is 
ration c 
bays an; 
that the 
straight 
years.
	        

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