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. A-320 amm pdf jgfkjgflkjgfdkjflkjgflkghfklghflkhfjglkghflkghfklglhflkghflkghflkhfkglhfklgflkghfkglkhfjlgflkghflkhjgflk. The rest of the year, we see how the ruddy ones got the better of the meteorologists, and how the meteorologists beat the ruddy ones. This is a simple graphic and may or may not be accurate, and does not reflect any changes in the physical conditions in the atmosphere (which is a complex thing) or satellite measurements (which are often volatile due to the difficulty of collecting data). 1 Actual seasonal variation in southern and northern hemispheres in summer, with zonal flow (a) and nocturnal flow (b) insolation. Also shown is the latitudinal average of the maximum zonal flow as a function of time of year. (c) Is shows the maximum in the zonal flow as a function of zonal angle at mid-latitudes. The zonal flow, which is the dominant mode of planetary wave structure, is more intense in the southern hemisphere in summer due to the higher insolation there and is also much weaker in winter due to the greater distance from the sun. (Image credit: Peter Read). You might be able to see something like this in the jet stream, which has a similar low-frequency period to the planetary wave. A seasonal cycle in jet-stream flow has also been observed at high altitudes in the atmosphere [ 43 ]. 1 The month-to-month satellite satellite winds anomaly for winter 2013–2014 is shown as a function of latitude. (Image credit: Royal Meteorological Society – Research). (a) The trend of the solar radiation is shown by satellite data as a function of latitude, with a warmer winter (blue line) and a cooler winter (red line) observed in winter 2014. It is clear that the impact of the winter was felt in the northern hemisphere, while the winter was slightly milder in the southern hemisphere. (b) The winter in the northern hemisphere was unusually weak in 2013–14, whilst the winter in the southern hemisphere was normal. 1 The August–November maximum in the jet stream is shown as a function of latitude. The figure illustrates that the maximum is strongly in the northern hemisphere, and as mentioned earlier, this

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