Climate in Brisbane, Queensland

The average temperature of the coastal strip is influenced by the warm waters of the Coral and Tasman Seas, which on the whole, keep the region free from extremes of temperature and offer moisture for precipitation. The yearly normal rainfall along the coastal strip is usually within the range of 1000 to 1600 millimeters. Escalating to over 3200 millimeters down parts of the northern Queensland coast near Innisfail.

The difference in climate across a region the size of Queensland is significant. little rainfall and scorching summers in the inland west, a heavy rain season in the north, and warm temperate conditions along the coastline distinguished with low minimum temperatures that can be experienced inland and about the southern ranges. Further to the west the land gradually flattens out to the dry inland plains. Here is where the hottest temperatures in the state most frequently occur during summer, and where the yearly norm rainfall drops below 200 millimeters. At the same time as tropical cyclones are a danger to coastal communities, they are a main supply of rain for the dry inla

On the western side of the Great Divide, the rainfall drops rapidly to a yearly norm of about 700 millimeters and then slowly but surely decreases more. In unison, average maximum temperatures progressively increase with escalating distance from the coastline. The mountains of the Great Dividing Range in Queensland achieve a maximum height of 1622 meters at Mt Bartle Frere near Innisfail, and there are more than a few peaks in surplus of 1000 meters, primarily in the north and southeast. The length of the Great Divide, the altitude suddenly amplifies away from the coastal plain, and then west of the Divide it slowly descends onto the western plains.