62 datasets found for "silo climate data"

Annual evaporation is typically much higher in inland parts of Queensland than in coastal and sub-coastal areas.

In Queensland, potential evaporation is much higher than mean annual rainfall in semi-arid inland locations.

2015 to 2019 was Queensland’s warmest 5-year period on record.

Coastal erosion continues to impact the Queensland coast, with several major incidents at developed areas.

Coastal erosion continues to impact the Queensland coast, with several major incidents at developed areas.

Coastal erosion continues to impact the Queensland coast, with several major incidents at developed areas.

2017 was Queensland’s warmest year on record. The years 2013 through to 2016 were also amongst the warmest on record.

This series contains input datasets used in the Revised Universal Soil Loss Equation (RUSLE). It is derived from soil data contained in the Australian Soil Resource Information...

Annual evaporation is typically much higher in inland parts of Queensland than in coastal and sub-coastal areas.

Drier than normal conditions prevailed across large parts of Queensland over the period from 2013 to 2019, with many areas experiencing drought.

Storm tide inundations continue to impact the coast.

While days with 'very heavy rainfall' are rare in parts of south-western Queensland, they are common along Queensland's north-eastern seaboard.

While days with ‘very heavy rainfall’ are rare in parts of south-western Queensland, they are common along Queensland’s north-eastern seaboard.

Storm tide inundations continue to impact the coast.

Queensland experienced 2 cyclones between March 2015 and December 2017.

Fire Regime Groups are groups of related regional ecosystems that share common fire management intent and are grouped for the purpose of practical fire management.

Queensland experienced 8 cyclones between 1 January 2018 and 1 April 2020.

Storm tide inundation events continue to impact the coast, however, no severe events were recorded for human settlements for 2012-2015.

El Niño conditions prevailed in 2015 and at the start of 2016, followed by ENSO-neutral conditions for much of 2017.

A transition occurred, from a La Niña in early 2012 to a strong El Niño during the second half of 2015.