Copyright © Philip M. Parker, INSEAD. Terms of Use.
| Domain | Definition |
Weather | An analytical technique to study the solar radiation incident on the Earth in which explicit calculations of atmospheric motions are omitted. In the zero- dimensional models, only the incoming and outgoing radiation is considered. The outgoing infrared radiation is a linear function of global mean surface air temperature, and the reflected solar radiation is dependent on the surface albedo. The albedo is a step function of the global meansurface air temperatures, and equilibrium temperatures are computed for a range of values of the solar constant. The one-dimensional models have surface air temperature as a function of latitude. At each latitude, a balance between incoming and outgoing radiation and horizontal transport of heat is computed. (Abbreviated as EBM.). (references) |
Source: compiled by the editor from various references; see credits. | |
Hexadecimal (or equivalents, 770AD-1900s) (references)45 4E 45 52 47 59 42 41 4C 41 4E 43 45 4D 4F 44 45 4C 53 |
| Leonardo da Vinci (1452-1519; backwards) (references)
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Binary Code (1918-1938, probably earlier) (references)01000101 01001110 01000101 01010010 01000111 01011001 00100000 01000010 01000001 01001100 01000001 01001110 01000011 01000101 00100000 01001101 01001111 01000100 01000101 01001100 01010011 |
HTML Code (1990) (references)E N E R G Y   B A L A N C E   M O D E L S |
ISO 10646 (1991-1993) (references)0045 004E 0045 0052 0047 0059 0042 0041 004C 0041 004E 0043 0045 004D 004F 0044 0045 004C 0053 |
Encryption (beginner's substitution cypher): (references)3948395241592363546354837392474938394653 |
| 1. Orthography 2. Bibliography |
Copyright © Philip M. Parker, INSEAD. Terms of Use.
