Many Auckland boaties head north for the summer break, up to the Bay of Islands and sometimes beyond, to the Cavalli Islands and Whangaroa Harbour. The prevailing southwest winds should mean a run up the coast. Right? Wrong. You need to know about the Northland lee trough.
Eight new trainees had their first day at MetService on January 25th 2017, welcomed by MetService and Victoria University staff, including MetService CEO, Peter Lennox and Victoria University's Associate Dean of Science, Shona De Sain.
Different parts of New Zealand are prone to different types of cloud. Use this handy guide to determine what types of cloud you get in your area, and where to go for some variety!
Near to the mountains
The word ‘storm’ is frequently misused in the media and colloquially, almost as much as the misuse of the term ‘weather bomb’*. In the strictest meteorological sense, a ‘storm’ is only a storm if accompanied by storm-force winds, which are defined by the Beaufort scale as having an average speed of over 47 knots (88 km/h). However, there are several other types of storm which don’t require storm-force winds.
Weather forecasting is basically an ‘initial value problem.’ This means that if weather models could capture the current weather perfectly i.e. correctly initialise the current state of the atmosphere, then in theory, they could forecast the future weather accurately well beyond the present limit of a week or so. After all, the atmosphere is a fluid, and follows strict laws of physics.
Here at MetService, people often send us photos of interesting clouds, unusual weather, and also atmospheric optical phenomena. Atmospheric optics is the branch of physics which describes how light interacts with the Earth’s atmosphere, to create a wide range of visual spectacles. Things such as rainbows, ice haloes, and crepuscular rays all come under atmospheric optics, along with many others. These can be observed all around New Zealand under the right conditions.
WEATHER BALLOON LAUNCH PROJECT - MetService, Space Place & Curious Minds NZ
By Lisa Murray, Communications Meteorologist.
Niko and Lucy launch the weather balloon at Paraparaumu workshop Friday 28th Oct 2016.
The photos in this blog were taken by MetService staff in August 2011.
Photo taken by Ian in Karori, a western suburb of Welington.
We’ve just come out of a cold, snowy spell – the most significant of this winter so far. Ski fields nationwide are well topped-up, the Tararua range has been textured with snow after a pretty bare winter, and parts of the central North Island continue to suffer the effects of substantial snowfalls and drifts.
Weather radars are used all around the world to detect rain, hail and snow, as it happens. However, there are times when the radar network can pick up other things as well. While you generally won't see aeroplanes on our radar images (the radar beam is usually beneath the flight path of most flights, and also our radars are calibrated to primarily pick up smaller objects, whereas radars at airports are calibrated differently to primarily pick up aeroplane-sized objects), there is a myriad of other things that can cause interference on our radar images, which I will explain in this blog.