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As displayed in the accompanying chart, Maribor has a temperate climate with warm summers and chilly winters. It lies in the northern hemisphere, so the temperatures peak in July and August. The temperature in Labuan, which lies near the equator, hardly changes through the year.
It lies in the northern hemisphere, so the temperatures peak in July and August. The temperature in Labuan, which lies near the equator, hardly changes through the year. Instead of summers and winters, there is a dry season in the beginning of the year, followed by a wet season with high rainfall.
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are A (tropical), B (arid), C (temperate), D (continental), and E (polar).
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. When combining the temperature and precipitation patterns together, we have even better clues as to the local ...
In practice, since temperature usually drops with altitude, the graphs are usually mostly vertical (see examples linked to below). The major use for skew-T log-P diagrams is the plotting of radiosonde soundings, which give a vertical profile of the temperature and dew point temperature throughout the troposphere and lower stratosphere.
The most commonly used form of the Köppen classification has five primary types labeled A through E. These primary types are A) tropical, B) dry, C) mild mid-latitude, D) cold mid-latitude, and E) polar. Tropical climates are defined as locations where the coolest monthly mean temperature is above 18 C (64.4 F).
A tephigram is one of a number [Note 1] of thermodynamic diagrams commonly used in weather analysis and forecasting. The name evolved from the original name "T- ϕ {\displaystyle \phi } -gram" to describe the axes of temperature (T) and entropy ( ϕ {\displaystyle \phi } ) used to create the plot. [ 1 ]
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