The Great Trigonometrical Survey of India

Table 1: A slow increase in accuracy. Meridional arc measurements during the 18th and 19th centuries.

Length of a degree(km)

Year

Observer

Country

Latitude of Middle arc(Deg/Sec)

111.49

1738

Maupertius - re-examined by Svanberg

Lapland

1.31.08 N

111.23

1802

Roy & Kater

England

52.35.45 N

111.11

1790

Delambre & Mecham

France

44.51.2 N

111.03

1755

Ruscovich

Rome

42.59.0 N

110.87

1750

Abb Lacaille

Cape of Good Hope

33.18.30 S

110.66

1835

Everest

India

16.7.22 N

110.64

1808

Lambton

India

2.32.21 N

110.58

1735

Condamine & Bouguer

Peru

1.31.08 N


Table 2: Official Ellipsoids Equatorial (Source: J. Snyder, Map Projections - A Working Manual). The Everest spheroid is still used in India, as well as in Pakistan, Nepal, Burma, Sri Lanka, Bangladesh, Bhutan, and other Southeast Asian countries. The Clarke (1866) ellipsoid was used for mapping in North America until recently. Many countries are now switching to WGS84, the datum used as a reference by the GPS.

Name

Date

Radius a (M)

Radius b (M)

Polar Flattening

WGS 84

1984

6,378,137

6,356,752.3

1/298.257

WGS 72

1972

6,378,135

6,356,750.5

1/298.26

Australian

1965

6,378,160

6,356,774.7

1/298.25

Krasovsky

1940

6,378,245

6,356,863

1/298.3

International

1924

6,378,388

6,356,911.9

1/297

Clarke

1880

6,378.249.1

6,356,514.9

1/293.46

Clarke

1866

6,378,206.4

6,356,583.8

1/294.98

Bessel

1841

6,377,397.2

6,356,079.0

1/299.15

Airy

1830

6,377,563.4

6,356,256.9

1/299.32

Everest

1830

6,377,276.3

6,356,075.4

1/300.8