攝氏

**攝氏度化換表**
由	化做	方程
攝氏	華氏（Fahrenheit）	°F = (°C × 1.8) + 32
華氏	攝氏	°C = (°F − 32) /1.8
攝氏	開爾文（Kelvin）	K = °C + 273.15
開爾文	攝氏	°C = K − 273.15
攝氏	蘭金（Rankine）	°R = (°C + 273.15) × 1.8
蘭金	攝氏	°C = (°R ÷ 1.8) – 273.15
以溫度距離來講， 1 °C = 1 K 、 1 °C = 1.8 °F 溫度轉換計算機

攝氏係一個表示溫度嘅系統，而攝氏度（符號 °C）就係用來表示攝氏比例裏面嘅其中一個距離，係一個度量衡。呢個度量衡可以用來表達一個確實嘅溫度，亦都可以表示兩個溫度之間嘅距離。攝氏呢個名係取自瑞典科學家安德斯攝爾修斯（Anders Celsius，1701年-1744年）嘅姓氏。攝爾修斯喺佢死之前兩年發明咗呢個度量衡。

1954年之前，攝氏零度同一百度分別定義咗做喺一個大氣壓力之下冰嘅熔點同埋水嘅沸點。呢個定義，而家嘅學校都重教緊。不過，1954年之後，國際協定將攝氏系統重新定義。絕對零度係 −273.15 °C，水嘅三相點就係 0.01 °C。呢度嘅水要指定係維也納標準海水（Vienna Standard Mean Ocean Water）。呢個定義將攝氏度同開爾文溫標呢個國際單位制基本單位直接連埋一齊，兩者嘅距離比例係一比一，每一點都相差273.15個單位。例如絕對零度，即係一個物質完全冇熱能嘅情況，係 −273.15 °C 同埋 0 K。

幾個攝氏制嘅重要溫度

	開爾文	攝氏	華氏
絕對零度（精確定義）	0 K	−273.15 °C	−459.67 °F
冰嘅熔點^[1]	273.15 K	0 °C	32 °F
水嘅三相點（精確定義）	273.16 K	0.01 °C	32.018 °F
水嘅沸點（大約）^[2]	373.1339 K	99.9839 °C	211.9710 °F

註腳

↑ The ice point of purified water has been measured to be 0.000 089(10) degrees Celsius - see Magnum, B.W. (1995). "Reproducibility of the Temperature of the Ice Point in Routine Measurements" (PDF). Nist Technical Note. 1411. 原著 (PDF)喺2007-03-07歸檔. 喺2007-02-11搵到. {{cite journal}}: Unknown parameter |month= ignored (help)
↑ For Vienna Standard Mean Ocean Water at one standard atmosphere (101.325 kPa) when calibrated solely per the two-point definition of thermodynamic temperature. Older definitions of the Celsius scale once defined the boiling point of water under one standard atmosphere as being precisely 100 °C. However, the current definition results in a boiling point that is actually 16.1 mK less. For more about the actual boiling point of water, see VSMOW in temperature measurement.

[1] The ice point of purified water has been measured to be 0.000 089(10) degrees Celsius - see Magnum, B.W. (1995). "Reproducibility of the Temperature of the Ice Point in Routine Measurements" (PDF). Nist Technical Note. 1411. 原著 (PDF)喺2007-03-07歸檔. 喺2007-02-11搵到. {{cite journal}}: Unknown parameter |month= ignored (help)

[2] For Vienna Standard Mean Ocean Water at one standard atmosphere (101.325 kPa) when calibrated solely per the two-point definition of thermodynamic temperature. Older definitions of the Celsius scale once defined the boiling point of water under one standard atmosphere as being precisely 100 °C. However, the current definition results in a boiling point that is actually 16.1 mK less. For more about the actual boiling point of water, see VSMOW in temperature measurement.

[1]

[2]