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1.3 FIGURE 1.3, dopicts a tropical cyclone in its mature stage. 1.5.1 Identify TWO Ractors from the diagram that were responsible for the: original dovelopment pf this tropical cyclone. \[ (2 \times 1) \] (2) 1.3.2 Refer to arsas \( A \) and 8 on the diagram. (a) Idenify areas A and B respectively. \[ (2 \times 1) \] (b) Diflerentiate between the air movements at areas A and B respectivaly, \[ (1 \times 2) \] (c) Mention the roasons for the differences in alr movements as stated in QUESTION 1.3.2(b). \[ (2 \times 1) \] 1.3.3 Draw a labelled synoptic map representation of the stage of the tropical cycione being dspicked by the diagram. \( (3 \times 1) \) (3) 1.3.4 Explain how the situation described at C on the diagram wn have a negative influence on the economy of the affocted corstal regions, \[ (2 \times 2) \]

Ask by Bernard Graham. in South Africa
Jan 29,2025

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**1.5.1 Identify TWO factors from the diagram that were responsible for the original development of this tropical cyclone.** *(2 × 1 = 2 marks)* **Answer:** 1. **Warm Sea Surface Temperatures:** Provide the necessary heat and moisture. 2. **Low Vertical Wind Shear:** Allows the cyclone to maintain its structure. --- **1.3.2 Refer to areas A and B on the diagram.** **(a) Identify areas A and B respectively.** *(2 × 1 = 2 marks)* **Answer:** - **Area A:** The **Eye** of the cyclone. - **Area B:** The **Eyewall** surrounding the eye. **(b) Differentiate between the air movements at areas A and B respectively.** *(1 × 2 = 2 marks)* **Answer:** - **Area A (Eye):** Sinking air movement. - **Area B (Eyewall):** Rising air movement. **(c) Mention the reasons for the differences in air movements as stated in QUESTION 1.3.2(b).** *(2 × 1 = 2 marks)* **Answer:** The Eye experiences sinking air due to high-pressure downdrafts, while the Eyewall has rising air from intense convection and thunderstorms. --- **1.3.3 Draw a labelled synoptic map representation of the stage of the tropical cyclone being depicted by the diagram.** *(3 × 1 = 3 marks)* **Answer:** *Include elements such as the low-pressure center, concentric isobars, symmetrical spiral rainbands, eye, and eyewall, all clearly labeled.* --- **1.3.4 Explain how the situation described at C on the diagram will have a negative influence on the economy of the affected coastal regions.** *(2 × 2 = 4 marks)* **Answer:** - **Damage to Infrastructure:** Storm surges and flooding can destroy buildings and disrupt utilities. - **Economic Disruption:** Businesses, agriculture, and tourism may be halted, leading to financial losses and reduced productivity.

Solution

**1.5.1 Identify TWO factors from the diagram that were responsible for the original development of this tropical cyclone.** *(2 × 1 = 2 marks)* **Answer:** 1. **Warm Sea Surface Temperatures:** Tropical cyclones typically form over ocean waters with temperatures exceeding 26.5°C, providing the necessary heat and moisture to fuel the storm. 2. **Low Vertical Wind Shear:** Minimal variation in wind speed and direction with height allows the cyclone to maintain its structure and intensify. --- **1.3.2 Refer to areas A and B on the diagram.** **(a) Identify areas A and B respectively.** *(2 × 1 = 2 marks)* **Answer:** - **Area A:** The **Eye** of the tropical cyclone, characterized by calm and clear conditions. - **Area B:** The **Eyewall**, which surrounds the eye and contains the most intense winds and thunderstorms. **(b) Differentiate between the air movements at areas A and B respectively.** *(1 × 2 = 2 marks)* **Answer:** - **Area A (Eye):** **Sinking (Subsiding) Air Movement** – Air descends, leading to stable and calm conditions. - **Area B (Eyewall):** **Rising (Ascending) Air Movement** – Air ascends rapidly, causing intense convection and strong thunderstorms. **(c) Mention the reasons for the differences in air movements as stated in QUESTION 1.3.2(b).** *(2 × 1 = 2 marks)* **Answer:** The **Eye (Area A)** experiences sinking air due to the high-pressure area formed by downdrafts from surrounding convection, leading to stable conditions. In contrast, the **Eyewall (Area B)** experiences rising air because of intense heating and moisture release from strong updrafts, sustaining vigorous thunderstorms and low-pressure dynamics. --- **1.3.3 Draw a labelled synoptic map representation of the stage of the tropical cyclone being depicted by the diagram.** *(3 × 1 = 3 marks)* **Answer:** *Since a drawing cannot be provided here, a synoptic map of a mature tropical cyclone would typically include:* - **Low-Pressure Center:** Represented at the center of the cyclone. - **Concentric Isobars:** Lines of equal pressure spiraling inward towards the center, indicating increasing wind speeds. - **Symmetrical Spiral Rainbands:** Extending outward from the center, showing areas of precipitation and thunderstorms. - **Eye and Eyewall:** The eye marked at the center with the surrounding eyewall depicted by tightly packed isobars. *Ensure all elements are clearly labeled to reflect the structure of a mature tropical cyclone.* --- **1.3.4 Explain how the situation described at C on the diagram will have a negative influence on the economy of the affected coastal regions.** *(2 × 2 = 4 marks)* **Answer:** Assuming **Point C** refers to the **Storm Surge** or **Heavy Flooding** associated with the tropical cyclone: 1. **Damage to Infrastructure:** Storm surges and flooding can devastate buildings, roads, bridges, and utility systems, leading to costly repairs and reconstruction efforts. 2. **Disruption of Economic Activities:** Essential services such as businesses, agriculture, fisheries, and tourism may be halted or severely impacted, resulting in financial losses and reduced economic productivity in the affected coastal regions. ---

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Tropical cyclones, such as hurricanes and typhoons, have fascinated scientists for centuries. Historically, these storms were often perceived as wrathful forces of nature, with cultures attributing them to divine intervention. The understanding of their formation and life cycle has evolved significantly since the 19th century, thanks in part to advancements in meteorology and satellite technology which allow us to study these massive storms in their full glory. In today's world, the real-world application of knowledge about tropical cyclones is crucial for disaster management and preparedness. Meteorologists use advanced models and satellite imaging to predict cyclone paths and intensity, allowing governments and organizations to issue timely warnings. This proactive approach can save lives, reduce economic losses, and ensure that communities are better prepared to respond when nature unleashes its fury!

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