Bridport 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 1995-2017 Average 9.8   18.5      
Nov 1995-2017 Highest 20.5 17th 2007 27.3 20th 2007    
Nov 1995-2017 Lowest 1.0 3rd 2014 12.0 8th 2013    
 
November 2024 Total         - 0 day(s)
Nov 1994-2017 Average Total         53.1 10.3 day(s)
Nov 1994-2017 Wettest Total         106.0 2001
Nov 1994-2017 Wettest 24hr Total         75.0 13th 2016
Nov 1994-2017 Driest Total         14.2 2007
 
Jan-Nov 2024 Total         - 0 day(s)
Jan-Nov 1994-2018 Average Total         706.2 137.5 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

BRIDPORT (SEA VIEW VILLAS)
Northeast, Tasmania
41.0025°S 147.3869°E 52m AMSL
Commenced 1994

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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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