Question map
Consider the following statements : 1. The Red Sea receives very little precipitation in any form. 2. No water enters the Red Sea from rivers. Which of the statements given above is/are correct ?
Explanation
The correct answer is option C because both statements are accurate.
**Statement 1 is correct:** The Red Sea region receives minimal precipitation, with annual rainfall varying between 100-200 mm in the north and dropping below 100 mm further[1] south except near the coast. This confirms that the Red Sea receives very little precipitation.
**Statement 2 is correct:** Perennial watercourses are absent in the Red Sea region, while surface drainage consists of ephemeral [2]streams and wadis. This means no permanent rivers discharge into the Red Sea. While there are major catchments like Khor Baraka, Arab, Arbaat–Odrus, Gowb and Diib[3], these are seasonal drainage systems, not permanent rivers that continuously flow into the Red Sea.
The Red Sea is therefore characterized by extremely low freshwater input, both from precipitation and river discharge, making it one of the world's most saline water bodies. Both statements accurately describe this hydrological characteristic.
Sources- [1] https://www.fao.org/4/i0936e/i0936e00.pdf
- [2] https://www.fao.org/4/ae917e/ae917e00.pdf
- [3] https://www.fao.org/4/ae917e/ae917e00.pdf
PROVENANCE & STUDY PATTERN
Full viewThis question masquerades as a specific fact-check but is actually a fundamental test of Oceanography (Salinity Budget). It penalizes students who rely solely on 'extreme statement' elimination tricks (e.g., 'No water' is usually false) without applying geographic common sense about the arid region surrounding the Red Sea.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
Gives a global classification of precipitation regimes (e.g., equatorial belt and coastal monsoon lands >200 cm; rain‑shadow and high latitudes <50 cm).
A student can locate the Red Sea on a world map, determine which of these precipitation regimes it lies in (coastal/monsoon/equatorial or arid/rain‑shadow), and therefore judge whether its mean annual precipitation is likely high (>200 cm), moderate, or very low (<50 cm).
Explains latitudinal patterns: between 45° and 65° N/S western continental margins get more rain; windward mountain coasts get greater rainfall—showing how latitude, winds and coastal mountains control coastal precipitation.
By placing the Red Sea in latitude and checking for prevailing wind patterns and nearby orography, a student can infer whether coastal rainfall there should be comparatively high or low.
Describes how equinox/ITCZ positions produce rainfall peaks in equatorial climates and that equatorial regions have annual averages always above 150 cm.
A student can check whether the Red Sea is influenced seasonally by the ITCZ/equatorial dynamics; if not, that suggests it would not share the high annual rainfall (>150 cm) typical of equatorial climates.
Gives examples of extreme orographic enhancement of precipitation (e.g., Mawsynram/Cherrapunji >1000 cm) showing that mountains near coasts can drastically increase local precipitation.
A student can examine whether the Red Sea coasts have comparable windward mountain topography; absence of such orographic features would make extreme high precipitation unlikely.
Notes that climate change projections include increased annual precipitation (but with fewer rainy days and higher intensity) and mentions sea‑level change—showing that regional precipitation can change over time.
A student considering modern versus historical averages could use this to ask whether recent trends might raise or alter reported Red Sea precipitation figures, prompting checking of time periods for any given average.
- Explicitly identifies the named catchments/khors in the Red Sea region, i.e. named watercourses that drain toward the Red Sea.
- Provides the actual names that can be listed as watercourses discharging to the Red Sea (Khor Baraka, Arab, Arbaat–Odrus, Gowb, Diib).
- States there are no perennial rivers in the project area but numerous ephemeral streams and wadis that provide surface drainage toward the Red Sea.
- Explains the hydrological context (ephemeral streams/wadis and the Red Sea Hills as a water divide) that indicates what discharges into the Red Sea in that region.
- Describes a fossil riverbed that had its origins in mountains bordering the eastern side of the present-day Red Sea, indicating historical river flow into the Red Sea region.
- Supports the idea that river channels (fossil/ancient) have drained toward the Red Sea area.
Mentions the East African Rift Valley extending along the Red Sea, giving a geographic feature that frames the Red Sea coast and its drainage context.
A student could use this to focus on rivers and drainage systems of countries along that rift/Red Sea margin (Ethiopia, Eritrea, Sudan, Egypt, Saudi Arabia, Yemen) to check for rivers that reach the Red Sea.
Gives examples of how specific rivers are associated with the particular seas they flow into (e.g., Yellow → Bohai Sea; Yangtze → East China Sea), illustrating the general principle of identifying a river's outlet by its coastal sea.
Apply the same principle: identify major rivers in Red Sea–bordering countries and check if their outlets lie on the Red Sea coast.
Defines what happens when a river reaches the sea (delta, distributaries), establishing physical signs to look for at a river mouth on any given sea coast.
Look along the Red Sea coast for deltas/estuaries or distributaries in maps or satellite images to spot rivers discharging there.
Explains that rivers generally discharge into the nearest ocean/sea (Bay of Bengal or Arabian Sea for Indian rivers), showing the useful rule of matching river flow direction and coastal adjacency to determine their outlet.
Use the adjacency rule: examine which rivers lie on coasts adjacent to the Red Sea and trace their downstream course to see if they reach the Red Sea.
Gives concrete examples of small coastal rivers discharging into a named sea (Arabian Sea), reinforcing that many short coastal rivers empty directly into the neighboring sea.
Similarly investigate short coastal streams/rivers on the Red Sea shoreline (by country) — many small rivers could directly discharge into the Red Sea and be identified on maps.
- [THE VERDICT]: Conceptual Sitter / Trap. While 'No water enters' sounds like an extreme statement (usually false), it is the defining geographic characteristic of the Red Sea found in standard Oceanography chapters (Factors affecting Salinity).
- [THE CONCEPTUAL TRIGGER]: Oceanography > Salinity & Temperature. Why is the Red Sea the most saline open sea in the world? Answer: High Evaporation + Very Low Precipitation + NO River Inflow.
- [THE HORIZONTAL EXPANSION]: Contrast the Red Sea's hydrology with other major basins: 1. Baltic Sea: Low salinity due to low evaporation + high river inflow/meltwater. 2. Black Sea: Positive water balance due to Danube/Dnieper inflow. 3. Mediterranean: Negative water balance (Evaporation > Precipitation/Runoff). 4. Persian Gulf: Receives the Shatt al-Arab (Tigris/Euphrates), unlike the Red Sea. 5. Caspian Sea: North is fresh (Volga inflow), South is saline.
- [THE STRATEGIC METACOGNITION]: Do not study maps in isolation. Overlay Climatology on Physical Geography. When looking at a sea, ask the 'Water Budget' questions: What flows in (Rivers)? What falls down (Rain)? What evaporates? This logic solves the question without needing to memorize specific river lists.
Annual precipitation is commonly categorized (e.g., >200 cm, 100–200 cm, 50–100 cm, <50 cm), which is the basic framework to estimate or compare rainfall over any region including seas.
High-yield for UPSC because classification lets you rapidly narrow plausible rainfall ranges by latitude and coastal context; links to world climate types, hydrology and biomes; enables questions that ask for comparative rainfall amounts or identification of climate regimes.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 24: Hydrological Cycle (Water Cycle) > World Distribution of Rainfall > p. 341
- FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 10: Water in the Atmosphere > World Distribution of Rainfall > p. 89
Topography forces air to rise, producing heavy precipitation on windward slopes and much reduced rainfall in leeward rain-shadow areas, a key process governing local annual totals.
Useful for explaining extreme local rainfall and contrasting nearby regions (coast vs interior); connects to monsoon dynamics, mountain geomorphology and regional climate questions; helps answer why adjacent locations can have very different annual precipitation.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 30: Climatic Regions > Precipitation > p. 431
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 24: Hydrological Cycle (Water Cycle) > World Distribution of Rainfall > p. 341
Monsoon systems can deliver the majority of a region's annual rainfall in a single season (sometimes >90%), strongly affecting annual totals and interannual variability.
Important for UPSC as many Indian and adjacent-region climate questions focus on monsoon distribution, seasonal impacts and variability; aids in solving questions on rainfall seasonality, agricultural implications and hydrological planning.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 4: Climate of India > RAINFALL DISTRIBUTION > p. 30
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 4: Climate of India > 1. Region of Very Heavy Rainfall > p. 37
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 4: Climate of India > VARIABILITY OF RAINFALL > p. 31
Indian rivers predominantly drain either into the Bay of Bengal or the Arabian Sea, defining regional drainage basins.
High-yield for UPSC geography: knowing which rivers flow to which oceanic outlets helps answer map and basin questions, compare climatic and sedimentary impacts, and link to regional economy and ports. This concept connects to river origins, course, and basin management questions.
- INDIA PHYSICAL ENVIRONMENT, Geography Class XI (NCERT 2025 ed.) > Chapter 3: Drainage System > Important Drainage Patterns > p. 19
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > 1.1 Consequent Rivers > p. 1
Rivers originating on the western slopes of the Western Ghats are short, swift and form a parallel drainage pattern discharging into the Arabian Sea.
Important for questions on drainage patterns, coastal geomorphology and river behavior in peninsular India; aids elimination of incorrect drainage destinations (e.g., distinguishing Arabian Sea from other seas).
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 16: Fluvial Landforms and Cycle of Erosion > Parallel Drainage Pattern > p. 215
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > 9. Parallel Drainage > p. 3
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > Mahi River > p. 19
The East African Rift extends along the Red Sea corridor up to Israel and Jordan, linking tectonics to regional drainage geometry.
Useful for continental-scale physical geography questions: ties tectonic structure to river courses and basin formation in East Africa and the Red Sea region; helps frame which rivers might plausibly drain into the Red Sea vs other basins.
- Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 9: Lakes > LAKES FORMED BY EARTH MOVEMENT > p. 81
The 'Suez Canal' connects the Red Sea to the Mediterranean, but biologically, the 'Lessepsian Migration' is the invasion of Red Sea marine species into the Mediterranean. The reverse rarely happens because the Red Sea is too salty and nutrient-poor for Atlantic/Mediterranean species.
Use the 'Nile Parallel' Logic. Visualize the map: The Nile River flows parallel to the Red Sea for thousands of kilometers but never enters it. Why? The 'Red Sea Hills' act as a massive drainage divide. If the longest river in the world, right next door, cannot breach the coast, it is logically consistent that no other significant rivers enter from that arid coastline.
Link to Economy & Environment (Mains GS-3): The absence of river water makes the Red Sea region the global hub for 'Desalination'. This connects to the 'Water-Energy Nexus' and the environmental challenge of 'Brine Disposal' affecting coral reefs in Saudi Arabia's NEOM project.