4. The Cuesta region (Sedimentary Najd)5. Aeolian Sands: an-Nafud, Ad-Dahna, Al-Jafurah, Ar-Rub’ al-Khali6. As-Summan and Widyan Plateaus7. <strong>Arabia</strong>n Gulf coastal region8. The Red Sea9. The <strong>Arabia</strong>n GulfClimate1. Rainfall<strong>Saudi</strong> <strong>Arabia</strong> is an area of dry, stable, subsiding air which gives rise to hot, dry and nearcloudless skies with dry days most of the year. Occasionally disturbed tropical monsoonweather may reach the Kingdom, bringing rain to the south of the country in the summer.In winter, remnants of the mid-latitude low pressure system may penetrate the north ofthe country giving rise to most rain in the region.Precipitation due to high altitude and proximity to the Red Sea augments rainfallalong the south-western escarpment. Daytime on-shore sea breezes force the moist airfrom the Red Sea to ascend, giving rise to afternoon showers and thunderstorms. Annualprecipitation in the mountains south of Taif is above 125 mm and may exceed 600 mm.Map 2.4 in Child and Granger (1990) shows the average annual precipitation in theKingdom. It is a guide as in most areas the precipitation is highly variable andunpredictable.2. Temperature and HumidityTemperatures are subject to considerable diurnal and seasonal fluctuations. Winters(December to February) are cool to warm. Summers (June to September) tend to be veryhot with temperatures above 40º C widespread and common and may approach 50º C.Humidity is generally low, except along the coasts where it may be quite high.Average August temperature in Jeddah 32º C but may reach 49º C, winter temperatureaverage 24º C, and relative humidity varies seasonally between 55% and 65%.Summer months in Riyadh are intensely hot with a daily maximum about 45º C. Wintersare cooler, with a maximum temperature of 22º C declining to 10º C or lower. Relativehumidity also varies with seasons with typical summer humidity of between 15 to 20 %.The Gulf coast is warm and humid in summer with average maximum of 42º Cand winter maximum average of 22º C. Humidity varies seasonally greatly from 40% insummer to about 70% in winter.The <strong>Arabia</strong>n GulfThe <strong>Arabia</strong>n Gulf extends from the Straits of Hormuz in the south to the Shatt al-Arab inthe north. It is a narrow sea, about 200 to 300 km wide and 1000 km long. It is mostlyquite shallow with an average depth of 35 m. the deepest water being found closer to theIranian coast (80m) and the Strait of Hormuz (100 m).Twenty thousand years ago, when the world was passing through an ‘ice age’,much of the water now in the sea was locked up in great ice sheets and the sea level wasabout 120 m lower than it is today. The Gulf was dry. The Tigris and Euphrates riversflowed along the coast of Iran and met the sea at the Strait of Hormuz. The sea onlyreached its present level about five thousand years ago. The plant and animal18
communities living in the Gulf have therefore only been here for a relatively short periodof time.The Gulf coastline ranges from extensive tidal mud flats at the head, forming thedelta of the Tigris and Euphrates, to the steep rocky Iranian coast, the rocky cliffs of theEmirates and the mountains of Oman. However, much of the west coast is relatively lowlying and extensive sand beaches and flats extend along the coast of <strong>Saudi</strong> <strong>Arabia</strong> andbeyond, both to the north and south. Numerous creeks or subkha break the westerncoastline: bays and small offshore islands are common.Water enters the <strong>Arabia</strong>n Gulf from the Indian Ocean through the Strait ofHormuz and flows north along the coast of Iran to Kuwait and then southerly down thecoast of <strong>Saudi</strong> <strong>Arabia</strong>. As the water follows an anticlockwise passage around the Gulf itbecomes saltier due to evaporation, and sinks below the less salty water.The Red SeaThe Red Sea is a narrow body of water approximately 130 kilometres long which is a partof the Red Sea – East African Rift System, where the African and the <strong>Arabia</strong>n tectonicplates diverge from each other. It lies between 30º N and 12º 30’ N, and between 32º30’E and 43º 30’E. In the south, it joins the Indian Ocean, and with construction of theSuez Canal connects with the Mediterranean Sea at the north of the Gulf of Suez. Themarine biota of the Red Sea has a complex biogeography and evolutionary history,related to tectonic activity and sea level changes over the past several million years.The maximum depth of the Red Sea is 2,850m, which is relatively deep for abody of water of its size. In the northern and central Red Sea a shallow coastal shelf mayextend only a few kilometres offshore, although in the southern Red Sea it is moreextensive. Excluding the coastal shallow areas, the average depth of the Red Sea is about700m and the main trough exceeds 1,000m.The Red Sea is a relatively young ocean, and its complex history hasencompassed some major environmental upheavals (Braithwate, 1987). It had its originin crustal sagging which occurred in the Mesozoic era, perhaps 180 million years ago, butonly became established as a distinct trough in the Oligocene, about 38 million years ago.During its formation the area was periodically covered by sea but was quite often dryland. A dramatic environmental change occurred in the later part of the Miocene period(from 25-5 million years ago) when the entire Red Sea basin became a great evaporationpan, forming considerable thickness of salt and other evaporate minerals. At the time theRed Sea was separated from the Indian Ocean by a neck of dry land, in the area where inStraits of Bab al Mandab now lie, but was linked across the Isthmus of Suez to theancient Mediterranean basin (part of the ancient Sea of Tethys).The Red Sea has unique coastal and marine environments in the world. Amongthe most notable is the extraordinary system of the coral reefs and their associatedanimals and plants. Surrounded by arid environments, which are themselves unique, theseenvironments support rich biological communities and representatives of severalendangered species. The natural resources have support coastal populations for thousandsof years, and nourished the development of a maritime and trading culture linking <strong>Arabia</strong>and Africa with Europe and Asia.The Red Sea is one of the most important repositories of marine biodiversity inthe world. Its relative isolation and physical conditions, which range from nearshoreshallows to depth of over 2000 meters in the Central rift, have given rise to anextraordinary range of ecosystems and biological diversity. Its most renowned expressionis the elaborate system of coral reefs. There are also mangroves, seagrass beds, reefs19