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The World Bank was created at the 1944 Bretton Woods Conference, along with the International Monetary Fund (IMF). The president of the World Bank is traditionally an American. [12] The World Bank and the IMF are both based in Washington, D.C., and work closely with each other.
The World Bank Institute is the capacity development branch of the World Bank, providing learning and other capacity-building programs to member countries. The IBRD has 189 member governments, and the other institutions have between 153 and 184. [2] The institutions of the World Bank Group are all run by a board of governors meeting once a year ...
A geographic coordinate system (GCS) is a spherical or geodetic coordinate system for measuring and communicating positions directly on Earth as latitude and longitude. [1] It is the simplest, oldest and most widely used type of the various spatial reference systems that are in use, and forms the basis for most others.
Geodetic latitude and geocentric latitude have different definitions. Geodetic latitude is defined as the angle between the equatorial plane and the surface normal at a point on the ellipsoid, whereas geocentric latitude is defined as the angle between the equatorial plane and a radial line connecting the centre of the ellipsoid to a point on the surface (see figure).
The graticule shows the latitude and longitude of points on the surface. In this example meridians are spaced at 6° intervals and parallels at 4° intervals. In geography, latitude is a coordinate that specifies the north–south position of a point on the surface of the Earth or another celestial body.
Between 2004 and 2013, the World Bank committed to lend or give at least $338 billion, according to bank data. Its private-lending affiliate, the International Finance Corporation, committed to invest at least $116 billion during the same period in corporations and other banks in pursuit of the overall goal of alleviating poverty.
A geodetic datum or geodetic system (also: geodetic reference datum, geodetic reference system, or geodetic reference frame, or terrestrial reference frame) is a global datum reference or reference frame for unambiguously representing the position of locations on Earth by means of either geodetic coordinates (and related vertical coordinates) or geocentric coordinates. [1]
The lines from pole to pole are lines of constant longitude, or meridians. The circles parallel to the Equator are circles of constant latitude, or parallels. The graticule shows the latitude and longitude of points on the surface. In this example, meridians are spaced at 6° intervals and parallels at 4° intervals.