Earth Science 7-Panama City, Panama
Panama City, Panama
Latitude/Longitude: 9 N 79 W [1]
Elevation: 15 meters [1]
Major Body of Water: Very near Caribbean Sea and Pacific Ocean [1]
Contents
Climate
Climate Zone
Af (tropical wet) according to Koppen Classification map [2] Other cities with similar climates include Suva, Figi Earth Sience 7-Suva, Fiji and Medan, Indonesia. Earth Science 7-Medan, Indonesia
Average Temperatures
' | Average Min Temp (⁰C) | Average Max Temp (⁰C) | Average Temperature (⁰C) |
January | 22 | 31 | 27 |
February | 22 | 32 | 27 |
March | 23 | 32 | 28 |
April | 23 | 32 | 28 |
May | 24 | 30 | 27 |
June | 24 | 30 | 27 |
July | 23 | 31 | 27 |
August | 24 | 30 | 27 |
September | 24 | 30 | 27 |
October | 23 | 29 | 26 |
November | 23 | 30 | 26 |
December | 23 | 31 | 27 |
Annual | 23 | 31 | 27 |
Average Precipitation
' | Average Wet Days (>0.1 mm) | Average Rainfall (mm) |
January | 4 | 48 |
February | 2 | 25 |
March | 2 | 10 |
April | 7 | 63 |
May | 17 | 239 |
June | 20 | 180 |
July | 17 | 199 |
August | 19 | 216 |
September | 20 | 200 |
October | 21 | 305 |
November | 20 | 268 |
December | 15 | 151 |
Factors That Regulate the Climate
Panama is about 8 degrees N, near the equator. This causes it to be very warm all year. It is sandwiched between the Caribbean Sea and the Pacific Ocean, making it very wet and humid most of the year.[1] The prevailing winds are usually from the North and the Northeast, but from the west during fall. Panama City has many forests due to its heavy rainfall.[4] It is in the ITCZ (intertropical convergence zone) belt of low pressure, also contributing to its heavy rain. [5]
Geology
Tectonic Plate Boundary
Panama is situated right on the border between the Caribbean Plate and the South American Plate.[6] This boundary is very complex, but it is believed to be a convergent boundary, with one plate subducting under the other.[7]
Rocks That Underlie Panama City
Although for the most part Panama's geology has not been explored in depth, a study over its geology is being conducted by the Smithsonian Tropical Research Institute. So far, they believe that millions of years ago mafic magma cooled in the region and became rock. After volcanoes stopped erupting in the area, sediments built up over the igneous rocks. These formed sedimentary rocks.[8]
- ↑ 1.0 1.1 1.2 1.3 Panama City, Panama. Map. Google Earth. Google.com, 6 Oct. 2010. Web. 6 Oct. 2010
- ↑ http://www.srh.noaa.gov/jetstream/global/climate_max.htm October 31
- ↑ 3.0 3.1 http://www.climatetemp.info/panama/ October 31
- ↑ http://www.atlapedia.com/online/countries/panama.htm October 31
- ↑ http://www.panama-guide.com/article.php/20081129133050126 November 12
- ↑ Spaulding, Nancy E. and Samuel N. Namowitz. Earth Science. Evanston IL: McDougal Littell Inc., 2005.
- ↑ http://gsa.confex.com/gsa/06boa/finalprogram/abstract_101391.htm February 16 Maria C. Guedez
- ↑ "The Panamá Geology Project." N.p., n.d. Web. 23 Feb. 2011. <http://striweb.si.edu/jaramillo/PDFs/Panama_Geology_Project.pdf>.