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Peak Hill Daily Summaries

June 2013
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date min to 9am anomaly max from 9am anomaly rain to 9am  
°C °C °C °C mm
Sat 01/06/2013 15.4 +9.3 18.1 +1.9 0.0  
Sun 02/06/2013 12.4 +6.3 15.5 -0.7 37.8  
Mon 03/06/2013 3.7 -2.4 15.9 -0.3 2.0  
Tue 04/06/2013 3.9 -2.2 18.3 +2.1 0.0  
Wed 05/06/2013 5.7 -0.4 17.4 +1.2 0.0  
Thu 06/06/2013 10.5 +4.4 17.0 +0.8 0.0  
Fri 07/06/2013 13.2 +7.1 17.3 +1.1 6.8  
Sat 08/06/2013 7.0 +0.9 19.4 +3.2 0.8  
Sun 09/06/2013 6.4 +0.3 20.0 +3.8 0.1  
Mon 10/06/2013 12.0 +5.9 17.6 +1.4 16.4  
Tue 11/06/2013 11.0 +4.9 20.2 +4.0 1.8  
Wed 12/06/2013 13.1 +7.0 17.3 +1.1 13.8  
Thu 13/06/2013 10.4 +4.3 15.3 -0.9 4.8  
Fri 14/06/2013 10.0 +3.9 12.9 -3.3 6.0  
Sat 15/06/2013 7.3 +1.2 14.6 -1.6 0.8  
Sun 16/06/2013 2.5 -3.6 15.6 -0.6 0.2  
Mon 17/06/2013 1.2 -4.9 14.3 -1.9 0.0  
Tue 18/06/2013 2.0 -4.1 12.0 -4.2 0.0  
Wed 19/06/2013 3.9 -2.2 15.0 -1.2 0.4  
Thu 20/06/2013 3.2 -2.9 16 +0 0.0  
 
June 2013 Average 7.7 +1.6 16.5 +0.3    
Jun 1966-2011 Average 6.1   16.2      
Jun 1966-2011 Highest 15.9 7th 2001 24.7 2nd 1994    
Jun 1966-2011 Lowest -2.5 15th 2006 7.0 26th 1989    
 
June 2013 Total         91.7 13 day(s)
Jun 1891-2011 Average Total         42.0 7.2 day(s)
Jun 1891-2011 Wettest Total         186.5 1916
Jun 1891-2011 Wettest 24hr Total         123.2 22nd 1925
Jun 1891-2011 Driest Total         0.0 1984
 
Jan-Jun 2013 Total         241.3 40 day(s)
Jan-Jun 1891-2012 Average Total         284.5 31.6 day(s)
 
Highlights the coolest minimum or maximum temperature during the period.
 
Highlights the warmest minimum or maximum temperature during the period.
 
Highlights the highest daily rainfall during the period.
10  
A yellow cell indicates a probable monthly record for this site (sites with ≥ 10 years of records only). The number of years of records available for the relevant field for this month is indicated in black. See the station's climate page for full details.

Station Details

PEAK HILL POST OFFICE
CW Slopes & Plains, New South Wales/ACT
32.7235°S 148.1902°E 285m AMSL
Commenced 1890

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