InitComponent::setSiteInfo() - CORE/lib.times/controllers/components/init.php, line 108
AppController::beforeFilter() - APP/app_controller.php, line 75
NewspapersController::beforeFilter() - CORE/lib.times/controllers/newspapers_controller.php, line 18
Controller::startupProcess() - CORE/cake-1.3.18/libs/controller/controller.php, line 522
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 188
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
Notice (8): Undefined variable: site_domain [CORE/lib.times/controllers/components/init.php, line 117]
InitComponent::setSiteInfo() - CORE/lib.times/controllers/components/init.php, line 117
AppController::beforeFilter() - APP/app_controller.php, line 75
NewspapersController::beforeFilter() - CORE/lib.times/controllers/newspapers_controller.php, line 18
Controller::startupProcess() - CORE/cake-1.3.18/libs/controller/controller.php, line 522
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 188
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
Notice (8): Undefined index: [CORE/lib.times/controllers/newspapers_controller.php, line 211]
$params = array(
"conditions" => array(
"Article.open_flag" => 1,
"Article.open_datetime <= " => "2026-04-23 17:48:43",
"Article.no" => "1275"
),
"fields" => array(
"ArticleSection.id",
"ArticleSection.code",
"ArticleSection.name",
"ArticleSection.context",
"Article.no",
"Article.title",
"Article.context_text",
"Article.level",
"Article.open_datetime",
"Article.academy"
),
"order" => array(
"Article.no" => "DESC"
)
)
$data = array(
"ArticleSection" => array(
"id" => "14",
"code" => "top",
"name" => "Headline News",
"context" => ""
),
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_datetime" => "2026-04-21 00:00:00",
"academy" => "6378",
"id" => "20707"
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
NewspapersController::index() - CORE/lib.times/controllers/newspapers_controller.php, line 211
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 205
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
Notice (8): Undefined index: [CORE/lib.times/controllers/newspapers_controller.php, line 212]
$params = array(
"conditions" => array(
"Article.open_flag" => 1,
"Article.open_datetime <= " => "2026-04-23 17:48:43",
"Article.no" => "1275"
),
"fields" => array(
"ArticleSection.id",
"ArticleSection.code",
"ArticleSection.name",
"ArticleSection.context",
"Article.no",
"Article.title",
"Article.context_text",
"Article.level",
"Article.open_datetime",
"Article.academy"
),
"order" => array(
"Article.no" => "DESC"
)
)
$data = array(
"ArticleSection" => array(
"id" => "14",
"code" => "top",
"name" => "Headline News",
"context" => ""
),
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_datetime" => "2026-04-21 00:00:00",
"academy" => "6378",
"id" => "20707",
"cover" => "/def.jpg"
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
NewspapersController::index() - CORE/lib.times/controllers/newspapers_controller.php, line 212
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 205
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
Notice (8): Undefined index: [CORE/lib.times/controllers/newspapers_controller.php, line 238]
$params = array(
"order" => array(
"ArticleSection.page" => "ASC",
"ArticleSection.sort_key" => "ASC"
),
"conditions" => array(
"Article.no" => "1275",
"Article.open_flag" => 1,
"ArticleSection.view_flag" => 1,
"Article.article_section_id <> " => 39,
"Article.open_datetime <= " => "2026-04-23 17:48:43"
),
"fields" => array(
"Article.no",
"Article.title",
"ArticleSection.app_code",
"Article.guide",
"Article.context_text",
"Article.level",
"Article.open_flag",
"ArticleSection.name",
"ArticleSection.enie_flag",
"ArticleSection.def_img",
"Article.academy"
)
)
$data = array(
"ArticleSection" => array(
"id" => "14",
"code" => "top",
"name" => "Headline News",
"context" => ""
),
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_datetime" => "2026-04-21 00:00:00",
"academy" => "6378",
"id" => "20707",
"cover" => "/def.jpg"
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
$list = array()
$size = 230
$val = array(
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"guide" => "",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_flag" => "1",
"academy" => "6378",
"id" => "20707"
),
"ArticleSection" => array(
"app_code" => "head",
"name" => "Headline News",
"enie_flag" => "1",
"def_img" => ""
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
$key = 0
NewspapersController::index() - CORE/lib.times/controllers/newspapers_controller.php, line 238
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 205
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
Notice (8): Undefined index: [CORE/lib.times/controllers/newspapers_controller.php, line 241]
$params = array(
"order" => array(
"ArticleSection.page" => "ASC",
"ArticleSection.sort_key" => "ASC"
),
"conditions" => array(
"Article.no" => "1275",
"Article.open_flag" => 1,
"ArticleSection.view_flag" => 1,
"Article.article_section_id <> " => 39,
"Article.open_datetime <= " => "2026-04-23 17:48:43"
),
"fields" => array(
"Article.no",
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"Article.guide",
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"Article.academy"
)
)
$data = array(
"ArticleSection" => array(
"id" => "14",
"code" => "top",
"name" => "Headline News",
"context" => ""
),
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_datetime" => "2026-04-21 00:00:00",
"academy" => "6378",
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),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
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)
$list = array()
$size = 230
$val = array(
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"guide" => "",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_flag" => "1",
"academy" => "6378",
"id" => "20707"
),
"ArticleSection" => array(
"app_code" => "head",
"name" => "Headline News",
"enie_flag" => "1",
"def_img" => ""
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
$key = 0
NewspapersController::index() - CORE/lib.times/controllers/newspapers_controller.php, line 241
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 205
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
Notice (8): Undefined index: [CORE/lib.times/controllers/newspapers_controller.php, line 328]
$params = array(
"conditions" => array(
"Article.article_section_id" => 14,
"Article.open_flag" => 1,
"Article.open_datetime <= " => "2026-04-23 17:48:43",
"Article.open_datetime BETWEEN ? AND ?" => array()
),
"fields" => array(
"Article.no",
"Article.open_datetime"
),
"order" => array(
"Article.open_datetime" => "ASC"
),
"recursive" => 0
)
$data = array(
"ArticleSection" => array(
"id" => "14",
"code" => "top",
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),
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_datetime" => "2026-04-21 00:00:00",
"academy" => "6378",
"id" => "20707",
"cover" => "/def.jpg"
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
$list = array(
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
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),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
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),
array(
"Article" => array(),
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),
array(
"Article" => array(),
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array(
"Article" => array(),
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array(
"Article" => array(),
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array(
"Article" => array(),
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),
array(
"Article" => array(),
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),
array(
"Article" => array(),
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"ArticleImg" => array(),
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),
array(
"Article" => array(),
"ArticleSection" => array(),
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array(
"Article" => array(),
"ArticleSection" => array(),
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),
array(
"Article" => array(),
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array(
"Article" => array(),
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array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
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array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
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)
)
$size = 230
$val = array(
"Article" => array(
"no" => "1273",
"open_datetime" => "2026-04-07 00:00:00",
"id" => "20677"
)
)
$key = 0
$app_enie = "enie_debate_1275"
$this_month = "2026-04"
$prev_month = "2026-03"
$next_month = "2026-05"
$nos = array(
"prev" => "2026-03",
"next" => "2026-05",
"year" => "2026",
"month" => "04"
)
NewspapersController::index() - CORE/lib.times/controllers/newspapers_controller.php, line 328
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 205
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
Notice (8): Undefined index: [CORE/lib.times/controllers/newspapers_controller.php, line 329]
$params = array(
"conditions" => array(
"Article.article_section_id" => 14,
"Article.open_flag" => 1,
"Article.open_datetime <= " => "2026-04-23 17:48:43",
"Article.open_datetime BETWEEN ? AND ?" => array()
),
"fields" => array(
"Article.no",
"Article.open_datetime"
),
"order" => array(
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"recursive" => 0
)
$data = array(
"ArticleSection" => array(
"id" => "14",
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"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_datetime" => "2026-04-21 00:00:00",
"academy" => "6378",
"id" => "20707",
"cover" => "/def.jpg"
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
$list = array(
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
)
)
$size = 230
$val = array(
"Article" => array(
"no" => "1273",
"open_datetime" => "2026-04-07 00:00:00",
"id" => "20677",
"cover" => "/def.jpg"
)
)
$key = 0
$app_enie = "enie_debate_1275"
$this_month = "2026-04"
$prev_month = "2026-03"
$next_month = "2026-05"
$nos = array(
"prev" => "2026-03",
"next" => "2026-05",
"year" => "2026",
"month" => "04"
)
NewspapersController::index() - CORE/lib.times/controllers/newspapers_controller.php, line 329
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 205
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
틴타임즈 1275호 (2026.04.21)｜틴타임즈 신문보기 :: 틴타임즈 - 구독률 1위 영자신문
if (Configure::read() > 0) { include ($___viewFn);
$___viewFn = "/home/www/lib.times/views/newspapers/index.ctp"
$___dataForView = array(
"rightad" => array(),
"videosection" => array(),
"sections" => array(
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array()
),
"title_for_layout" => "틴타임즈 1275호 (2026.04.21)｜틴타임즈 신문보기",
"d" => DvalueComponent
DvalueComponent::$datetime = array
DvalueComponent::$fn = array
DvalueComponent::$info = array
DvalueComponent::$publish_weekday = array
DvalueComponent::$magazines = array
DvalueComponent::$site_code = array
DvalueComponent::$small_name = array
DvalueComponent::$full_name = array
DvalueComponent::$samples = array
DvalueComponent::$pay = array
DvalueComponent::$level = array
DvalueComponent::$enie = array
DvalueComponent::$video = array
DvalueComponent::$enabled = true,
"meta" => array(
"keyword" => array(),
"des" => "",
"etc" => array()
),
"titles" => array(
array()
),
"popup" => array(),
"nos" => array(
"prev" => "2026-03",
"next" => "2026-05",
"year" => "2026",
"month" => "04",
"articles" => array()
),
"data" => array(
"ArticleSection" => array(),
"Article" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
"list" => array(
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array(),
array()
),
"bottomad" => array(),
"firstad" => array(
"Advertisement" => array()
),
"thisweek" => array(
"Article" => array()
)
)
$loadHelpers = true
$cached = false
$common = commonHelper
commonHelper::$helpers = NULL
commonHelper::$base = ""
commonHelper::$webroot = "/"
commonHelper::$theme = NULL
commonHelper::$here = "/newspapers/index/Article.no:1275"
commonHelper::$params = array
commonHelper::$action = "index"
commonHelper::$plugin = NULL
commonHelper::$data = NULL
commonHelper::$namedArgs = NULL
commonHelper::$argSeparator = NULL
commonHelper::$validationErrors = NULL
commonHelper::$tags = array
commonHelper::$__tainted = NULL
commonHelper::$__cleaned = NULL
$time = TimeHelper
TimeHelper::$helpers = NULL
TimeHelper::$base = ""
TimeHelper::$webroot = "/"
TimeHelper::$theme = NULL
TimeHelper::$here = "/newspapers/index/Article.no:1275"
TimeHelper::$params = array
TimeHelper::$action = "index"
TimeHelper::$plugin = NULL
TimeHelper::$data = NULL
TimeHelper::$namedArgs = NULL
TimeHelper::$argSeparator = NULL
TimeHelper::$validationErrors = NULL
TimeHelper::$tags = array
TimeHelper::$__tainted = NULL
TimeHelper::$__cleaned = NULL
$krTime = krTimeHelper
krTimeHelper::$helpers = array
krTimeHelper::$def_date = "0000-00-00 00:00:00"
krTimeHelper::$base = ""
krTimeHelper::$webroot = "/"
krTimeHelper::$theme = NULL
krTimeHelper::$here = "/newspapers/index/Article.no:1275"
krTimeHelper::$params = array
krTimeHelper::$action = "index"
krTimeHelper::$plugin = NULL
krTimeHelper::$data = NULL
krTimeHelper::$namedArgs = NULL
krTimeHelper::$argSeparator = NULL
krTimeHelper::$validationErrors = NULL
krTimeHelper::$tags = array
krTimeHelper::$__tainted = NULL
krTimeHelper::$__cleaned = NULL
krTimeHelper::$Time = TimeHelper object
$session = SessionHelper
SessionHelper::$helpers = array
SessionHelper::$__active = true
SessionHelper::$valid = false
SessionHelper::$error = false
SessionHelper::$_userAgent = ""
SessionHelper::$path = "/"
SessionHelper::$lastError = NULL
SessionHelper::$security = "low"
SessionHelper::$time = 1776934124
SessionHelper::$sessionTime = 1776952124
SessionHelper::$cookieLifeTime = 1080000
SessionHelper::$watchKeys = array
SessionHelper::$id = NULL
SessionHelper::$host = NULL
SessionHelper::$timeout = NULL
SessionHelper::$base = ""
SessionHelper::$webroot = "/"
SessionHelper::$here = "/newspapers/index/Article.no:1275"
SessionHelper::$params = array
SessionHelper::$action = "index"
SessionHelper::$data = NULL
SessionHelper::$theme = NULL
SessionHelper::$plugin = NULL
$sort = sortHelper
sortHelper::$sort = ""
sortHelper::$direction = "asc"
sortHelper::$named = false
sortHelper::$helpers = NULL
sortHelper::$base = ""
sortHelper::$webroot = "/"
sortHelper::$theme = NULL
sortHelper::$here = "/newspapers/index/Article.no:1275"
sortHelper::$params = array
sortHelper::$action = "index"
sortHelper::$plugin = NULL
sortHelper::$data = NULL
sortHelper::$namedArgs = NULL
sortHelper::$argSeparator = NULL
sortHelper::$validationErrors = NULL
sortHelper::$tags = array
sortHelper::$__tainted = NULL
sortHelper::$__cleaned = NULL
$text = TextHelper
TextHelper::$helpers = NULL
TextHelper::$base = ""
TextHelper::$webroot = "/"
TextHelper::$theme = NULL
TextHelper::$here = "/newspapers/index/Article.no:1275"
TextHelper::$params = array
TextHelper::$action = "index"
TextHelper::$plugin = NULL
TextHelper::$data = NULL
TextHelper::$namedArgs = NULL
TextHelper::$argSeparator = NULL
TextHelper::$validationErrors = NULL
TextHelper::$tags = array
TextHelper::$__tainted = NULL
TextHelper::$__cleaned = NULL
$form = FormHelper
FormHelper::$helpers = array
FormHelper::$fieldset = array
FormHelper::$__options = array
FormHelper::$fields = array
FormHelper::$requestType = NULL
FormHelper::$defaultModel = NULL
FormHelper::$_inputDefaults = array
FormHelper::$_lastAction = ""
FormHelper::$base = ""
FormHelper::$webroot = "/"
FormHelper::$theme = NULL
FormHelper::$here = "/newspapers/index/Article.no:1275"
FormHelper::$params = array
FormHelper::$action = "index"
FormHelper::$plugin = NULL
FormHelper::$data = NULL
FormHelper::$namedArgs = NULL
FormHelper::$argSeparator = NULL
FormHelper::$validationErrors = NULL
FormHelper::$tags = array
FormHelper::$__tainted = NULL
FormHelper::$__cleaned = NULL
FormHelper::$Html = HtmlHelper object
$javascript = JavascriptHelper
JavascriptHelper::$useNative = true
JavascriptHelper::$enabled = true
JavascriptHelper::$safe = false
JavascriptHelper::$tags = array
JavascriptHelper::$_blockOptions = array
JavascriptHelper::$_cachedEvents = array
JavascriptHelper::$_cacheEvents = false
JavascriptHelper::$_cacheToFile = false
JavascriptHelper::$_cacheAll = false
JavascriptHelper::$_rules = array
JavascriptHelper::$__scriptBuffer = NULL
JavascriptHelper::$helpers = NULL
JavascriptHelper::$base = ""
JavascriptHelper::$webroot = "/"
JavascriptHelper::$theme = NULL
JavascriptHelper::$here = "/newspapers/index/Article.no:1275"
JavascriptHelper::$params = array
JavascriptHelper::$action = "index"
JavascriptHelper::$plugin = NULL
JavascriptHelper::$data = NULL
JavascriptHelper::$namedArgs = NULL
JavascriptHelper::$argSeparator = NULL
JavascriptHelper::$validationErrors = NULL
JavascriptHelper::$__tainted = NULL
JavascriptHelper::$__cleaned = NULL
$html = HtmlHelper
HtmlHelper::$tags = array
HtmlHelper::$_crumbs = array
HtmlHelper::$__includedScripts = array
HtmlHelper::$_scriptBlockOptions = array
HtmlHelper::$__docTypes = array
HtmlHelper::$helpers = NULL
HtmlHelper::$base = ""
HtmlHelper::$webroot = "/"
HtmlHelper::$theme = NULL
HtmlHelper::$here = "/newspapers/index/Article.no:1275"
HtmlHelper::$params = array
HtmlHelper::$action = "index"
HtmlHelper::$plugin = NULL
HtmlHelper::$data = NULL
HtmlHelper::$namedArgs = NULL
HtmlHelper::$argSeparator = NULL
HtmlHelper::$validationErrors = NULL
HtmlHelper::$__tainted = NULL
HtmlHelper::$__cleaned = NULL
$ajax = AjaxHelper
AjaxHelper::$helpers = array
AjaxHelper::$Html = HtmlHelper object
AjaxHelper::$Javascript = JavascriptHelper object
AjaxHelper::$callbacks = array
AjaxHelper::$ajaxOptions = array
AjaxHelper::$dragOptions = array
AjaxHelper::$dropOptions = array
AjaxHelper::$sortOptions = array
AjaxHelper::$sliderOptions = array
AjaxHelper::$editorOptions = array
AjaxHelper::$autoCompleteOptions = array
AjaxHelper::$__ajaxBuffer = array
AjaxHelper::$base = ""
AjaxHelper::$webroot = "/"
AjaxHelper::$theme = NULL
AjaxHelper::$here = "/newspapers/index/Article.no:1275"
AjaxHelper::$params = array
AjaxHelper::$action = "index"
AjaxHelper::$plugin = NULL
AjaxHelper::$data = NULL
AjaxHelper::$namedArgs = NULL
AjaxHelper::$argSeparator = NULL
AjaxHelper::$validationErrors = NULL
AjaxHelper::$tags = array
AjaxHelper::$__tainted = NULL
AjaxHelper::$__cleaned = NULL
AjaxHelper::$Form = FormHelper object
$rightad = array()
$videosection = array()
$sections = array(
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
),
array(
"ArticleSection" => array()
)
)
$title_for_layout = "틴타임즈 1275호 (2026.04.21)｜틴타임즈 신문보기"
$d = DvalueComponent
DvalueComponent::$datetime = array
DvalueComponent::$fn = array
DvalueComponent::$info = array
DvalueComponent::$publish_weekday = array
DvalueComponent::$magazines = array
DvalueComponent::$site_code = array
DvalueComponent::$small_name = array
DvalueComponent::$full_name = array
DvalueComponent::$samples = array
DvalueComponent::$pay = array
DvalueComponent::$level = array
DvalueComponent::$enie = array
DvalueComponent::$video = array
DvalueComponent::$enabled = true
$meta = array(
"keyword" => array(),
"des" => "",
"etc" => array()
)
$titles = array(
array(
"name" => "틴타임즈 신문보기",
"link" => "/newspapers/index"
)
)
$popup = array()
$nos = array(
"prev" => "2026-03",
"next" => "2026-05",
"year" => "2026",
"month" => "04",
"articles" => array(
array(),
array(),
array()
)
)
$data = array(
"ArticleSection" => array(
"id" => "14",
"code" => "top",
"name" => "Headline News",
"context" => ""
),
"Article" => array(
"no" => "1275",
"title" => "Arctic Sea Ice Ties Record Low at Winter Peak",
"context_text" => "Arctic sea ice appears to have reached its seasonal winter maximum on March 15, matching the lowest level in the satellite record and aligning with conditions observed in 2025. The result extends a decades-long decline and reflects continuing structural changes across the polar region.
Data from the National Snow and Ice Data Center and NASA show the ice expanded to approximately 14.29 million square kilometers at its peak. That figure remains well below the 1981-2010 average, leaving a deficit roughly equal to twice the size of the state of Texas. The difference between 2025 (14.31 million square kilometers) and 2026 is minimal and falls within the margin of measurement uncertainty, so the two years are treated as effectively tied.
The longer-term trend is more significant. Since 1979, Arctic sea ice has steadily diminished, and winter growth no longer offsets losses during warmer months. This shift suggests a system that is gradually losing its capacity to recover.
Surface extent alone does not fully capture current conditions. Researchers increasingly emphasize ice thickness and composition, which better indicate how well the ice can withstand seasonal stress. These factors provide a clearer measure of overall stability than area alone.
A large share of today’s ice cover consists of first-year ice, which forms each winter and melts more easily. It is thinner and less durable than older ice, making it more vulnerable to rising temperatures. Multi-year ice, once widespread across the Arctic, has declined sharply, weakening the overall structure of the ice pack.
Measurements show total ice volume in March 2026 fell to a record low, roughly 15% lower than the levels recorded just two years earlier. This rapid loss leaves the ice entering the summer melt season in a fragile state, where thinner layers are more likely to fracture and melt quickly.
Regional conditions also contributed to this year’s outcome. The Barents Sea and the Sea of Okhotsk experienced delayed freeze-up and reduced ice coverage. Warmer ocean temperatures slowed formation and limited consolidation.
Exposed ocean absorbs more solar energy than reflective ice, amplifying warming through the albedo effect. This process accelerates melting and makes it harder for ice to reform, reinforcing a cycle of continued loss.
The final extent in September will depend on weather conditions in the months ahead. Even so, the winter peak already signals an Arctic that is thinner, less stable, and increasingly vulnerable to ongoing warming.
",
"level" => "4",
"open_datetime" => "2026-04-21 00:00:00",
"academy" => "6378",
"id" => "20707",
"cover" => "/def.jpg"
),
"Video" => array(),
"ArticleImg" => array(
array(),
array()
),
"ArticleQuestion" => array()
)
$list = array(
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
),
array(
"Article" => array(),
"ArticleSection" => array(),
"Video" => array(),
"ArticleImg" => array(),
"ArticleQuestion" => array()
)
)
$bottomad = array()
$firstad = array(
"Advertisement" => array(
"img" => "<img src="http://news.timescore.co.kr/files/uploads//" alt="" title="" />"
)
)
$thisweek = array(
"Article" => array(
"no" => "1275",
"id" => "20707"
)
)
include - CORE/lib.times/views/newspapers/index.ctp, line 4
View::_render() - CORE/cake-1.3.18/libs/view/view.php, line 736
View::render() - CORE/cake-1.3.18/libs/view/view.php, line 431
Controller::render() - CORE/cake-1.3.18/libs/controller/controller.php, line 909
Dispatcher::_invoke() - CORE/cake-1.3.18/dispatcher.php, line 208
Dispatcher::dispatch() - CORE/cake-1.3.18/dispatcher.php, line 172
[main] - APP/webroot/index.php, line 88
