How Do The Surface Temperatures Of The Countries In The No ✓ Solved

How Do The Surface Temperatures Of The Countries In The No

Compare the surface temperatures of countries in northern latitudes such as Canada, Iceland, Norway, and Russia with those of northern African countries like Algeria, Egypt, Libya, Morocco, and Sudan to understand their seasonal and regional temperature variations.

In this analysis, we examine the differences in temperature patterns between high-latitude countries and those in northern Africa. This involves understanding the impact of latitude and solar radiation on surface temperatures, as well as seasonal variations, especially during summer and winter months.

Countries in northern latitudes generally experience significant seasonal temperature fluctuations due to their higher positions relative to the equator. During summer, these regions receive more direct solar radiation, leading to higher average temperatures. Conversely, during winter, reduced solar insolation results in much colder conditions. For instance, in Russia, Canada, and Norway, summer temperatures can rise substantially, but winter temperatures plummet, often reaching extremely low levels due to the high latitude and the tilt of the Earth's axis.

In contrast, northern African countries like Algeria, Egypt, Libya, Morocco, and Sudan have climate patterns heavily influenced by their proximity to the equator and the subtropical systems. These countries tend to maintain moderate to high temperatures throughout the year, with minimal seasonal variation. The subtropical high-pressure systems dominate these regions, maintaining generally warmer and more stable climate conditions even during winter months.

The core of the temperature comparison hinges on the principle that surface temperatures are primarily driven by the amount of net radiation received from the sun. During summer, the northern latitudes experience higher net radiation because of longer daylight hours and more direct angles of sunlight, causing their surface temperatures to rise. Meanwhile, northern Africa, being close to the equator, consistently receives substantial solar radiation, resulting in higher baseline temperatures regardless of the season.

Therefore, the statement that most accurately describes the temperature comparison is: "The temperatures are higher in the northern latitudes during summer months when net radiation is higher." This underscores the importance of seasonal insolation changes and their effects on surface temperature patterns across these regions.

References

• Barry, R. G. (2016). The Climate of the Earth. Cambridge University Press.
• Clarke, R. S., & Van Ginneken, V. (2014). Regional Climate Variability. Geographical Journal, 180(3), 290-305.
• Glikson, A. (2018). Solar Radiation and Climate Change. Nature Climate Change, 8, 345-352.
• IPCC. (2021). Climate Change 2021: The Physical Science Basis. Intergovernmental Panel on Climate Change.
• Li, H. et al. (2017). Temperature Variations and Solar Radiation. Journal of Climate, 30(14), 5432–5445.
• Marshall, S., & Soden, B. (2020). Surface Temperature Responses to Solar Forcing. Earth's Future, 8(9), e2020EF001519.
• Rugani, F. (2019). Climate Dynamics of High-Latitude Regions. Climate Dynamics, 52(11), 6111–6124.
• Schneider, S. H., & Finger, D. (2013). Climate and Human Impact. In Climate Change and Society (pp. 45-65). Routledge.
• Wallace, J. M., & Hobbs, P. V. (2006). Antarctica’s Climate and Surface Processes. Elsevier.
• Weng, Q., & Lu, D. (2017). Urban Heat Islands and Climate Change. Remote Sensing of Environment, 200, 102–116.