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Atlantic Hurricane Calm: High Ocean Temperatures Not Enough

Atlantic Hurricane Calm: High Ocean Temperatures Not Enough

September 18, 2025 Ahmed Hassan - World News Editor World

Here’s a⁢ breakdown⁣ of the⁣ text,‌ focusing on the key details and⁤ its institution:

Overall Topic: ‌The unusually quiet⁣ Atlantic hurricane season in ⁤2024.

Key Points:

* Low Hurricane Activity: ⁢the⁢ Atlantic hurricane season has⁣ been remarkably inactive so far.
* Cause: Dry ⁢Air & Wind Shear: the primary reason ‍is a combination of‍ factors:
* ‍ ‍ High⁣ Subtropical Pressure: Record high air pressure in the ⁣subtropics.
‍ *⁤ Dry Air Inflow: This ⁤pressure‍ system⁣ is pushing dry desert air into the tropics.
⁤ * ⁢ Dry Spring in Africa: A dry⁢ spring in Africa contributed to‌ the conditions.
‌ * ‍⁤ Increased ‌Vertical Wind Shear: Stronger vertical‌ wind ‍shear is suppressing⁣ tropical convection (the formation‌ of storms).
* Saharan ⁣Dust: ​An unusually⁤ large amount of Saharan ⁢dust has been transported across the Atlantic, further suppressing storm progress.
* ⁣ ⁤ Potential for Change: There’s still a month and a ‌half left ⁢in ⁢the ​hurricane season, and strong hurricanes can ⁣form late in ‌the season (as seen in ⁢the previous year with Hurricanes Helene and Milton).

Structure:

  1. Image & Caption: A map showing ocean surface⁢ temperature anomalies in⁣ 2024, with ‌a ⁢caption attributing⁣ the photo​ to C3S/ECMWF.
  2. Description of Causes (3 paragraphs): ⁤ ‍ These paragraphs detail the ‌atmospheric conditions leading ⁤to the quiet season. They explain⁢ the interplay of pressure systems,‍ dry air, wind shear, and Saharan⁤ dust.
  3. Outlook⁤ (1 paragraph): ‌‌ This section offers ⁣a cautious note,stating that⁣ the season isn’t over and ⁤late-season storms are possible.
  4. Twitter Quote: A truncated Twitter quote is present at the end.

In essence, the article explains why the 2024 ‍Atlantic hurricane season has been unusually calm, attributing it to ‌specific atmospheric conditions, ⁢while​ also acknowledging the possibility of late-season storm development.

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