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We could also derive information about a site's ecological conditions through a climograph. For example, if precipitation is consistently low year-round, we might suggest the location reflects a desert; if there is a noticeable seasonal pattern to the precipitation, we might suggest the location experiences a monsoon season.
name = Christchurch, New Zealand Name used in the default map caption; image = Christchurch, New Zealand map.svg The default map image, without "Image:" or "File:" top = -43.4 Latitude at top edge of map, in decimal degrees; bottom = -43.65 Latitude at bottom edge of map, in decimal degrees; left = 172.45 Longitude at left edge of map, in ...
The blue numbers are the amount of precipitation in either millimeters (liters per square meter) or inches. The red numbers are the average daily high and low temperatures for each month, and the red bars represent the average daily temperature span for each month. The thin gray line is 0 °C or 32 °F, the point of freezing, for orientation.
Climate charts provide an overview of the climate in a particular place. The letters in the top row stand for months: January, February, etc. The bars and numbers convey the following information: The blue bars represent the average amount of precipitation (rain, snow etc.) that falls in each month. The blue numbers are the amount of ...
Christchurch (/ ˈ k r aɪ s. tʃ ɜːr tʃ / ⓘ; Māori: Ōtautahi) is the largest city in the South Island and the second-largest city by urban area population in New Zealand. [a] Christchurch has an urban population of 415,100, and a metropolitan population of over half a million.
The Google Chart API allows a variety of graphs to be created. Livegap Charts creates line, bar, spider, polar-area and pie charts, and can export them as images without needing to download any tools. Veusz is a free scientific graphing tool that can produce 2D and 3D plots. Users can use it as a module in Python.
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The key facts to emerge are that New Zealand did experience a noticeable cooler climate, but at a slightly later date than in the Northern Hemisphere. [22] The onset of cooler climate was about 1450 and lasted until 1850. Indications are that temperatures were in the range of 1.5-2.0 degree Celsius lower than present during the New Zealand LIA.