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This study explores the pressure levels at 300 mb, 500 mb, and 1000 mb within Earth's atmosphere, focusing on meridional and zonal flows. We analyze the typical 500 mb chart, highlighting the relationship between wind speed and pressure gradients, and illustrate the behavior of the mid-latitude jet stream. The dynamics of pressure aloft, especially at varying latitudes (0°N, 45°N, 90°N), are crucial for understanding weather patterns and the movement of systems. This research provides insights into atmospheric pressure variances and the impact on climate systems.
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300 mb 300 mb 500 mb 500 mb 1000 mb 1000 mb PRESSURE ALOFT Top of Atmosphere 300 mb 500 mb 1000 mb Earth’s surface 0oN 45oN 90oN
Tall Blocks Short Blocks PRESSURE ALOFT
PRESSURE ALOFT 90oN 45oN 0oN 5200 5400 5600 5800
PRESSURE ALOFT 90oN 45oN 0oN 5200 5400 5600 5800
PRESSURE ALOFT 90oN 45oN 0oN 5200 5400 5600
PRESSURE ALOFT 5800 5760 5700 5640 5580 5520 5460 5400 5340 5280 HL
HL PRESSURE ALOFT 5800 5760 5700 5640 5580 5520 5460 5400 5340 5280
GEOSTROPHIC WIND 5300 5500 5700
TYPICAL 500mb CHART Note wind speed/pressure gradient relationship!
MID-LATITUDE JET Pressure = 250 mb Pressure = 250 mb X 10000 m Wedge of Cold Air 60oN 30oN