{"id":3808,"date":"2024-02-22T21:05:05","date_gmt":"2024-02-23T02:05:05","guid":{"rendered":"https:\/\/oceanweatherservices.com\/blog\/?p=3808"},"modified":"2024-02-22T21:05:05","modified_gmt":"2024-02-23T02:05:05","slug":"la-nina-azores-bermuda-ridge-impact-2024-hurricane-season","status":"publish","type":"post","link":"https:\/\/oceanweatherservices.com\/blog\/2024\/02\/22\/la-nina-azores-bermuda-ridge-impact-2024-hurricane-season\/","title":{"rendered":"La Ni\u00f1a and the Azores-Bermuda Ridge: Impact on the 2024 Hurricane Season"},"content":{"rendered":"<h2><\/h2>\n<div id=\"attachment_3810\" style=\"width: 372px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Dorian.jpg\"><img aria-describedby=\"caption-attachment-3810\" decoding=\"async\" loading=\"lazy\" class=\" wp-image-3810\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Dorian-300x209.jpg\" alt=\"\" width=\"362\" height=\"252\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Dorian-300x209.jpg 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Dorian.jpg 679w\" sizes=\"(max-width: 362px) 100vw, 362px\" \/><\/a><p id=\"caption-attachment-3810\" class=\"wp-caption-text\">Catagory 5 Hurricane Dorian<\/p><\/div>\n<h2><b>Introduction<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">During the 2023 hurricane season, a strong El Ni\u00f1o event had significant effects on the Azores-Bermuda Ridge, leading to a weakening of this high-pressure system. As a result, surface winds, especially in the tropical Atlantic, decreased. This reduction in surface winds had several consequences, including unusual sea surface warming due to decreased ocean mixing and evaporation. Additionally, other factors, such as a strong \u00a0<a href=\"https:\/\/climatedataguide.ucar.edu\/climate-data\/atlantic-multi-decadal-oscillation-amo\">Atlantic Multi-decadal Oscillation (AMO)<\/a>, reduced sulfate particles from cleaner shipping fuels, the Hunga-Tonga volcanic eruption, and lower levels of African dust, may have contributed to the overall climate conditions.<\/span><\/p>\n<div id=\"attachment_3812\" style=\"width: 637px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164049.png\"><img aria-describedby=\"caption-attachment-3812\" decoding=\"async\" loading=\"lazy\" class=\"size-full wp-image-3812\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164049.png\" alt=\"\" width=\"627\" height=\"421\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164049.png 627w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164049-300x201.png 300w\" sizes=\"(max-width: 627px) 100vw, 627px\" \/><\/a><p id=\"caption-attachment-3812\" class=\"wp-caption-text\">June 2023 Surface Pressure Anomaly<\/p><\/div>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">In this analysis, I will explore the transition from El Ni\u00f1o to La Ni\u00f1a and its potential<\/span><span style=\"font-weight: 400;\"> impact on the 2024 hurricane season.<\/span><\/p>\n<h2><b>La Ni\u00f1a and Wind Shear<\/b><\/h2>\n<h3><b>El Ni\u00f1o to La Ni\u00f1a Transition<\/b><\/h3>\n<p><span style=\"font-weight: 400;\">Currently, El Ni\u00f1o is weakening rapidly, and meteorologists anticipate the development of a La Ni\u00f1a event by the main 2024 hurricane season. La Ni\u00f1a is characterized by cooler-than-average sea surface temperatures in the central and eastern tropical Pacific Ocean. Just how will this transition affect the Atlantic hurricane environment?<\/span><\/p>\n<h3><b>Wind Shear and Tropical Cyclones<\/b><\/h3>\n<p><span style=\"font-weight: 400;\">During La Ni\u00f1a events, wind shear in the tropical Atlantic typically decreases. Wind shear refers to the change in wind speed and direction with altitude. Reduced wind shear creates favorable conditions for the development and intensification of tropical cyclones. With weaker wind shear, disturbances in the tropics can organize more effectively, potentially leading to stronger storms.<\/span><\/p>\n<h2><b>The Strengthened Azores-Bermuda Ridge<\/b><\/h2>\n<h3><b>Trade Winds and Storm Paths<\/b><\/h3>\n<p><span style=\"font-weight: 400;\">La Ni\u00f1a tends to strengthen the Azores-Bermuda Ridge, a high-pressure system located in the North Atlantic. As this ridge strengthens, trade winds increase. These trade winds play a crucial role in steering tropical cyclones. Here\u2019s how:<\/span><\/p>\n<ol>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Westward Movement: A stronger Azores-Bermuda Ridge tends to steer Atlantic tropical cyclones farther west. This westward shift increases the risk of landfalls in regions such as the Caribbean, the US East Coast, and the Gulf Coast.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Trade Wind Enhancement: Stronger trade winds enhance ocean surface mixing. This process involves cooler water from deeper ocean layers rising to the surface. Consequently, the sea surface temperatures may gradually cool during the hurricane season.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Evaporation and Moisture Transport: The intensified winds also lead to increased evaporation and moisture transport. This contributes to further cooling of the sea surface.<\/span><\/li>\n<\/ol>\n<div id=\"attachment_3814\" style=\"width: 699px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164119.png\"><img aria-describedby=\"caption-attachment-3814\" decoding=\"async\" loading=\"lazy\" class=\"wp-image-3814 size-full\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164119.png\" alt=\"\" width=\"689\" height=\"253\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164119.png 689w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-164119-300x110.png 300w\" sizes=\"(max-width: 689px) 100vw, 689px\" \/><\/a><p id=\"caption-attachment-3814\" class=\"wp-caption-text\">Azores-Bermuda Ridge controls Tropical Cyclone Tracks<\/p><\/div>\n<h2><\/h2>\n<h2><\/h2>\n<h2><\/h2>\n<h2><b>Sea Surface Temperature Anomalies<\/b><\/h2>\n<h3><b>Outlook for 2024<\/b><\/h3>\n<p><span style=\"font-weight: 400;\">Given the current very high sea surface temperature anomaly in the tropical North Atlantic, it is likely to remain above normal as we move into the peak of the 2024 hurricane season. However, the strengthening La Ni\u00f1a and the associated changes in wind patterns may gradually mitigate this anomaly.<\/span><\/p>\n<div id=\"attachment_3815\" style=\"width: 874px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-204719.png\"><img aria-describedby=\"caption-attachment-3815\" decoding=\"async\" loading=\"lazy\" class=\"size-full wp-image-3815\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-204719.png\" alt=\"\" width=\"864\" height=\"549\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-204719.png 864w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-204719-300x191.png 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2024\/02\/Screenshot-2024-02-22-204719-768x488.png 768w\" sizes=\"(max-width: 864px) 100vw, 864px\" \/><\/a><p id=\"caption-attachment-3815\" class=\"wp-caption-text\">Tropical North Atlantic Sea Surface Temperatre Anomaly<\/p><\/div>\n<p><span style=\"font-weight: 400;\">In summary, the transition from El Ni\u00f1o to La Ni\u00f1a could significantly influence the behavior of tropical cyclones in the Atlantic. If the Azores-Bermuda Ridge strengthens during this hurricane season we can expect an increased risk of tropical cyclone landfalls in regions such as the Caribbean, the US East Coast, and the Gulf Coast. As wind shear decreases, tropical cyclone frequency and intensity can increase so it will be essential to stay informed about the evolving conditions and their potential impact on hurricane activity.<\/span><\/p>\n<p><a href=\"https:\/\/oceanweatherservices.com\/blog\/maritime-weather-experts\/\"><b>Ocean Weather Service<\/b><\/a><\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Currently, El Ni\u00f1o is weakening rapidly, and meteorologists anticipate the development of a La Ni\u00f1a event by the main 2024 hurricane season. La Ni\u00f1a is characterized by cooler-than-average sea surface temperatures in the central and eastern tropical Pacific Ocean. Just how will this transition affect the Atlantic hurricane environment? <a href=\"https:\/\/oceanweatherservices.com\/blog\/2024\/02\/22\/la-nina-azores-bermuda-ridge-impact-2024-hurricane-season\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[1],"tags":[43,21,18,27,9,5,14,111],"_links":{"self":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3808"}],"collection":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/comments?post=3808"}],"version-history":[{"count":4,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3808\/revisions"}],"predecessor-version":[{"id":3817,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3808\/revisions\/3817"}],"wp:attachment":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/media?parent=3808"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/categories?post=3808"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/tags?post=3808"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}