Premium
The effect of freezing and melting processes on the daily temperature curve at quebec city
Author(s) -
Longley Richmond W.
Publication year - 1949
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1002/qj.49707532506
Subject(s) - snow , environmental science , maximum temperature , atmospheric sciences , climatology , thermodynamics , materials science , meteorology , geography , physics , geology
A study was made of the frequency distribution of the daily maximum and minimum temperatures for the city of Quebec for the periods 1 February to 31 May and 1 September to 31 December. It was discovered that during the period when the snow was melting there was a damping effect of approximately 2°F on the maximum temperature on those days when the temperature rose above freezing. After the snow disappeared and the ground thawed out, there was a corresponding damping of about 1°F on the minimum temperature on those days when it approached freezing. The damping effect in the autumn is less than 1°F. Other features of these frequency distributions are also brought out.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom