Terrain
Most of the Jordan's surface is composed of a desert plateau in the east and high lands in the west. The Great Grotto Valley is separated between the two banks: the eastern and the western parts of the Jordan River. The Jordan surface consists of three regions: the Jordan Valley low-pitched groove, mountain heights, and Al-Badia desert plateau.
Climate and geographical structure
The climate of Jordan is a combination of both climates: the Mediterranean basin and arid desert, where the Mediterranean climate prevails in the north and west of the country, while the desert climate prevails in most of the country. All in all, the weather is hot and dry in the summertime and mild and humid in the winter. There is a climatic diversity in Jordan, where the dry tropical climate prevails in the Jordan Valley, while the warm steppes climate in the mountainous highlands, the Mediterranean climate in the mountainous highlands, and the cold Mediterranean climate prevailing in the high mountain peaks such as Ajloun, Steppes climate on the eastern slopes, and dry desert climate in the eastern Badia.
Annual temperatures range between 12-25 ° C (54-77 ° F), and are highest in the summer to fourties (105- 115 ° F) in desert areas. Rainfall ranges from 50 mm (1.97 inches) per year in the desert around 580 mm (22.8 inches) in the northern highlands. Snow falls at low intervals on most of the mountainous highlands in the north, central and southern kingdom, and is very abundant and sometimes accumulated.