Murrurundi Daily Summaries

November 2024
icon icon icon icon
date min to 9am anomaly max from 9am anomaly rain to 9am  
°C °C °C °C mm
Fri 01/11/2024 - - - - -  
Sat 02/11/2024 - - - - -  
Sun 03/11/2024 - - - - -  
Mon 04/11/2024 - - - - -  
Tue 05/11/2024 - - - - -  
Wed 06/11/2024 - - - - -  
Thu 07/11/2024 - - - - -  
Fri 08/11/2024 - - - - -  
Sat 09/11/2024 - - - - -  
Sun 10/11/2024 - - - - -  
Mon 11/11/2024 - - - - -  
Tue 12/11/2024 - - - - -  
Wed 13/11/2024 - - - - -  
Thu 14/11/2024 - - - - -  
Fri 15/11/2024 - - - - -  
Sat 16/11/2024 - - - - -  
Sun 17/11/2024 - - - - -  
Mon 18/11/2024 - - - - -  
Tue 19/11/2024 - - - - -  
Wed 20/11/2024 - - - - -  
Thu 21/11/2024 - - - - -  
Fri 22/11/2024 - - - - -  
 
November 2024 Average -   -      
Nov 1965-2018 Average 10.9   26.4      
Nov 1965-2018 Highest 25.1 22nd 2009 40.6 23rd 2014    
Nov 1965-2018 Lowest 0.0 3rd 2003 10.7 19th 1986    
 
November 2024 Total         - 0 day(s)
Nov 1870-2018 Average Total         75.9 7.8 day(s)
Nov 1870-2018 Wettest Total         347.6 2000
Nov 1870-2018 Wettest 24hr Total         117.6 20th 2000
Nov 1870-2018 Driest Total         0.8 1897
 
Jan-Nov 2024 Total         - 0 day(s)
Jan-Nov 1870-2019 Average Total         733.5 79.9 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

MURRURUNDI (HAYDON STREET)
Hunter, New South Wales/ACT
31.7678°S 150.8418°E 467m AMSL
Commenced 1870 / Closed 2019

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Nature?s air conditioner: how the seabreeze will help Sydney cope during the heatwave

14:37 AEDT As heatwave conditions take hold of southeastern Australia this weekend, the cooling seabreeze will be crucial in easing daytime heat, but how does it form? During periods with weak synoptic forcing, with a broad high pressure system moving slowly over the Tasman Sea, the seabreeze circulation dominates, as we can see below.

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