Its Mediterranean climate has
average maximum temperatures between 14C and 28C and average minimums between 7C and 16C.
Not exact matches
Whilst extreme
temperatures are rare, January and February tend to be Scotland's coldest months although still mild with daytime
maximum temperatures averaging between 5 ° to 7 °C.
On a seasonal basis the ranges
between the daily
maximum, minimum and
average are all listed and the lowest ratio is that the daily minimum
temperature range over the year is 77,000 times greater than the
temperature difference that would result from the proposed 30 % reduction in emissions.
Sourced from The Climate of Western Australia 1876 - 1899 by Government Astronomer W. Ernest Cooke, below are monthly
average maximum and minimum
temperature comparions
between Perth's first official weather recording station and the Perth Metro 9225 station at Mt Lawley.
Figure 16.2: Projected number of days per year with a
maximum temperature greater than 90 °F
averaged between 2041 and 2070, compared to 1971 - 2000, assuming continued increases in global emissions (A2) and substantial reductions in future emissions (B1).
In contrast, meteorological data collected from three nearby coastal stations (Brevoort Island, Cape Dyer, and Resolution Island)
between 1950 and 1992 indicated that the mean minimum and
maximum air
temperatures for the month of April are normally 10 - 20 °C cooler than the
averages we recorded at our camp.
As for the
temperature maximum between 600 and 800 yr A.D., we can see that the majority of points in the short - lived trees are well above the
average, while in the 20th century they tend to gravitate to the lower part of the graph
Analysing the mean summer
maximum temperature differences
between Bourke and Charleville, the unadjusted data (Figure 5) indicates that Bourke was, on
average, about 2 °C warmer prior to Stevenson screen installation in 1908 than it was in the years following that, with wide year - to - year variations.
An Australian example is the comparison
between a Stevenson screen and a Glaisher stand carried out
between 1887 and 1947 at Adelaide (Nicholls et al., 1996), which found that
maximum temperatures in the Glaisher stand were about 0.6 °C warmer than those in the Stevenson screen as an annual
average, with differences of about 1 °C in summer.