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West Roebuck Sky Observations
- observations list type
- observations
- sky observations
| time | vis | cloud | current weather | past weather | |
|---|---|---|---|---|---|
| m | |||||
| Mon 06:00 WST |
- | - | - | - | |
| Sun 18:00 WST |
- | - | - | - |
|
| Sun 17:00 WST |
- | - | - | - | |
| Sun 16:00 WST |
- | - | - | - | |
| Sun 15:00 WST |
- | - | - | - | |
| Sun 04:00 WST |
- | - | - | - | |
| Sun 03:00 WST |
- | - | 190TS | - | |
| Sun 02:00 WST |
- | - | - | - | |
| Sat 15:00 WST |
- | - | 190TS | - | |
| Sat 14:00 WST |
- | - | - | - | |
| Sat 13:00 WST |
- | - | - | - | |
| Fri 15:00 WST |
- | - | - | - | |
| Fri 14:00 WST |
- | - | - | - | |
| Fri 13:00 WST |
- | - | - | - | |
| Fri 12:00 WST |
- | - | - | - | |
| Thu 18:00 WST |
- | - | 126TS | - |
|
| Thu 17:00 WST |
- | - | - | - | |
| Thu 16:00 WST |
- | - | - | - | |
| Thu 15:00 WST |
- | - | - | - | |
| Thu 14:00 WST |
- | - | - | - | |
| Thu 13:00 WST |
- | - | - | - | |
| Wed 19:00 WST |
- | - | - | - | |
| Wed 18:00 WST |
- | - | - | - | |
| Wed 17:00 WST |
- | - | - | - | |
| Wed 16:00 WST |
- | - | - | - | |
| Wed 15:00 WST |
- | - | - | - | |
| Wed 13:00 WST |
- | - | - | - | |
| Wed 04:00 WST |
- | - | - | - | |
| Wed 03:00 WST |
- | - | - | - | |
| Wed 02:00 WST |
- | - | - | - | |
| Wed 01:00 WST |
- | - | - | - | |
| Wed 00:00 WST |
- | - | - | - |
|
| Tue 18:00 WST |
- | - | 126TS | - | |
| Tue 17:00 WST |
- | - | - | - | |
| Tue 16:00 WST |
- | - | - | - | |
| Tue 15:00 WST |
- | - | - | - | |
| Tue 14:00 WST |
- | - | - | - | |
| Tue 13:00 WST |
- | - | - | - | |
| Tue 07:00 WST |
- | - | - | - |
Station Details
WEST ROEBUCK
Kimberley, Western Australia
Kimberley, Western Australia
17.8964°S 122.3122°E
32m AMSL
Commenced 1999
Commenced 1999
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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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