The effects of sea level rise come in many forms. During tropical storms, higher sea levels drive intense storm surges — water level much higher than normal tides. But with sea level rise, the tides themselves can cause flooding.
During high-tide floods, water can make its way from the ocean onto land and bubble up from storm drains. In cities like Miami & Annapolis, high-tide flooding can close down streets & businesses, and damage infrastructure like pipes & wastewater systems. go.nasa.gov/3eISZj9
Between 2000-2015, days with high-tide flooding doubled along the U.S. Northeast Atlantic coast, & that will likely keep climbing. Some locations could see high-tide flooding 180 days a year by 2050. From May '19 to April '20, Annapolis had a record 18 days of high-tide flooding.
The most significant driver of this type of flooding is sea level rise, but the tides themselves — caused by the pull of the Moon’s gravity — along with local weather and regional climate patterns also affect when the flooding occurs.
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We know that as human activity warms the planet, global sea level is rising. We know that about 2/3 of sea level rise so far has come from melting ice. But how do we know this? We can measure it from space. #SeeingTheSeas
Sea level isn’t uniform around the planet. Tides and currents, the density and temperature of water, and landforms can affect where the ocean piles up. We know this because we measure the shape of the ocean using radar altimetry. go.nasa.gov/3n0EpGB
Altimetry works by bouncing radio waves off the ocean surface and timing how quickly they return. Then comes the next challenge: Calculating the natural and seasonal changes in ocean height to determine how much more global warming has made seas rise.
Sea levels on the West Coast of the United States are rising at a faster rate than the global average – and that trend is likely to continue for at least a few years, with likely effects for people living in the region. #SeeingTheSeas go.nasa.gov/3n2Kxy7
The height of the sea surface in the western and eastern tropical Pacific Ocean seesaws over time – when one is higher, the other is lower. This is driven on shorter timescales by two natural climate patterns: the El Niño-Southern Oscillation and the Pacific Decadal Oscillation.
Every few years, the El Niño Southern Oscillation (ENSO) pattern produces either an El Niño or a La Niña event. El Niños can increase West Coast sea level; while La Niñas can decrease it.
#HurricaneDelta was the 25th named Atlantic storm of the 2020 hurricane season. After exhausting a list of prepared names, @WMO turns to the Greek alphabet to name storms.
Hurricanes typically get a massive boost of energy when they pass over warm waters. #HurricaneDelta rapidly intensified to a Category 4 storm. #HurricaneLaura also underwent rapid intensification in the Gulf of Mexico. go.nasa.gov/2GTxb7V
As it made landfall, #HurricaneDelta was generating heavy rainfall. Combining data from @NASARain’s satellites with computer models helps track precipitation to help those living in the storm’s path. go.nasa.gov/3dlIXnr
Arctic sea ice reached its second-lowest minimum extent on record on Sept. 15, 2020. This year’s extent was larger only than 2012’s extent. @NASA and @NSIDC track sea ice through the year. go.nasa.gov/33LwmFH
Sea ice plays an important role in keeping our planet cool. Light-colored ice reflects heat from the Sun back into the atmosphere, while darker ocean water absorbs it, so warming accelerates as sea ice extent declines.
Sea ice extent grows and shrinks with the seasons, with the colder northern winter temperatures freezing sea water and the warmer summer temperatures melting it. Over the last decades, sea ice extent has been trending smaller — a direct result of warmer global temperatures.
318 gigatons.
That’s how much ice is lost every year from Antarctica and Greenland’s ice sheets, according to new science from @NASA_Ice's #ICESat2. go.nasa.gov/3cb0bCC
But… how much ice is that, really? 🤔
Let's say 🧊= a gigaton of ice.
🧊 would be enough to cover NYC’s Central Park in ice past the top of the Chrysler Building. When melted, it would fill 400,000 Olympic-sized swimming pools.
Each year from 2003 to 2019, Greenland lost 200 🧊s. Antarctica lost 118 🧊s.
From 2003-2019, Greenland lost: 🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊🧊
2019 was the second hottest 🌡 year and the last decade was the warmest decade on record. The global average temperature was more than 2°F warmer than during the late 19th century. go.nasa.gov/2RnffDZ
Scientists at @NASA and @NOAA separately analyze temperature measurements taken at thousands of weather stations, ships and ocean buoys around the globe. Although the records differ slightly due to data processing, they both show a long-term pattern 📈 of increasing temperature.
The global temperature 🌎 is an average, so not every place on Earth had its second-warmest year. For instance, the continental U.S. had a cold October, but Alaska set records for high temperatures. The U.S. was still warmer than average over the year.