 | 1840 - 702 str.
...of the sea. These experiments are very Important in relation to Ute theory of physical climate: — 1. The temperature of the ocean is generally lower at mid-day than that of the atmosphere, noticed in the shade. 2 Itlsalnrs higher at midnight. 3. In the morning and the evening, these two... | |
 | 1840 - 698 str.
...of the sea. These experiments are very important in relation to the theory of physical climate :— 1. The temperature of the ocean Is generally lower at mid-day than that of the atmosphere, noticed In the shade. 2. It ia always higher at midnight. 3. In the morning and the evening, these... | |
 | Perry Fairfax Nursey - 1840 - 706 str.
...of the sea. These experiments are very important In relation to the theory of physical climate :— 1. The temperature of the ocean is generally lower at mid-day than that of the atmosphere, noticed in the shade. 2 It is always higher at midnight. 3. In the morning and the evening, these two... | |
 | James Laurie - 1842 - 1098 str.
...of the sea. These experiments arc very important in relation to the theory of physical climate : — 1. The temperature of the ocean is generally lower at mid-day than that of the atmosphere, noticed in the shade. 2. It is always higher at midnight. 3. In the morning and the evening, these... | |
 | System - 1842 - 894 str.
...of the sea. These experiments an; very important in relation to the theory of physical climate: — 1. The temperature of the ocean is generally lower at mid-day than that of the atinospherc, noticed in the shade. 2. It i« always higher at midnight. 3. In the morning and the evening,... | |
 | Thomas Milner - 1850 - 604 str.
...general conclusions of interest upon this point may be stated : — 1 . The temperature of the surface of the ocean is generally lower at midday than that of the atmosphere noticed in the shade. 2. It is always higher at midnight. 3. Morning and evening the two temperatures... | |
 | George William Fitch - 1856 - 276 str.
...temperature of the ocean the following facts have been deduced : 1 . The temperature of the surface of the ocean is generally lower at mid-day than that of the atmosphere in the shade. 2. It is always higher at midnight. 3. Morning and evening the two temperatures usually correspond. 4. The mean... | |
 | George William Fitch - 1856 - 274 str.
...the temperature of the ocean the following facts have been deduced: 1. The temperature of the surface of the ocean is generally lower at mid-day than that of the atmosphere in the shade. 2. It is always higher at midnight. 3. Morning and evening the two temperatures usually correspond. 4. The mean... | |
 | George William Fitch - 1856 - 280 str.
...temperature of the ocean the following facts have been deduced : 1 . The temperature of the surface of the ocean is /generally lower at mid-day than that of the atmosphere in the shade.V 2. /It is always higher at midnight.X 3. (Morning and eveningi the two temperatures usually... | |
 | Thomas Milner - 1876 - 818 str.
...general conclusions of interest upon this point may be stated : — 1. The temperature of the surface of the ocean is generally lower at midday than that of the atmosphere noticed in the shade. 2. It is always higher at midnight. 3. Morning and evening the two temperatures... | |
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These experiments arc very important in relation to the theory of physical climate : — 1. The temperature of the ocean is generally lower at mid-day than that of the atmosphere, noticed in the shade. 2. It is always higher at midnight. 3. In the morning... 