Lucinda Point 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 - - - - -  
Sat 23/11/2024 - - - - -  
 
November 2024 Average -   -      
Nov 1980-2020 Average 24.2   28.4      
Nov 1980-2020 Highest 28.5 28th 2018 34.4 28th 2018    
Nov 1980-2020 Lowest 20.4 4th 2009 23.9 27th 1999    
 
November 2024 Total         - 0 day(s)
Nov 1980-2019 Average Total         77.9 8.2 day(s)
Nov 1980-2019 Wettest Total         607.4 2010
Nov 1980-2019 Wettest 24hr Total         132.0 2nd 2013
Nov 1980-2019 Driest Total         0.0 2019
 
Jan-Nov 2024 Total         - 0 day(s)
Jan-Nov 1980-2020 Average Total         975.8 114.1 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

LUCINDA POINT
Lower Burdekin, Queensland
18.5203°S 146.3861°E 10m AMSL
Commenced 1980

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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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