Copyright © Philip M. Parker, INSEAD. Terms of Use.
| Domain | Definition |
Weather | Thermodynamic models that determine the equilibrium temperature distribution for an atmospheric column and the underlying surface, subject to prescribed solar radiation at the top of the atmosphere and prescribed atmospheric composition and surface albedo. Submodels for the transfer of solar and terrestrial radiation, the heat exchange between the earth's surface and atmosphere, the vertical redistribution of heat within the atmosphere, the atmospheric water vapor content and clouds are included in these one-dimensional models. Abbreviated as RCM. (references) |
Source: compiled by the editor from various references; see credits. | |
Hexadecimal (or equivalents, 770AD-1900s) (references)52 41 44 49 41 54 49 56 45 2D 43 4F 4E 56 45 43 54 49 56 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)01010010 01000001 01000100 01001001 01000001 01010100 01001001 01010110 01000101 00101101 01000011 01001111 01001110 01010110 01000101 01000011 01010100 01001001 01010110 01000101 00100000 01001101 01001111 01000100 01000101 01001100 01010011 |
HTML Code (1990) (references)R A D I A T I V E - C O N V E C T I V E   M O D E L S |
ISO 10646 (1991-1993) (references)0052 0041 0044 0049 0041 0054 0049 0056 0045 002D 0043 004F 004E 0056 0045 0043 0054 0049 0056 0045 004D 004F 0044 0045 004C 0053 |
Encryption (beginner's substitution cypher): (references)52353843355443563915374948563937544356392474938394653 |
| 1. Orthography 2. Bibliography |
Copyright © Philip M. Parker, INSEAD. Terms of Use.
