Highlights

High Latitudes

 «» 
1 2 3 4

"Let us love winter, for it is the spring of genius." - Pietro Aretino

Climate is changing. And nowhere is it more evident than near Earth's poles. Life that has adapted to these extreme regions – including sea ice-dependent species from tiny algae to huge polar bears – is being impacted. Salinity is a "key ingredient" for high-latitude ocean ecological communities. Why? It affects seawater density which, in turn, influences the movement of water, heat, and carbon.

A basin surrounded by land, the Arctic Ocean has a cap of frozen seawater (a.k.a. "sea ice") that waxes and wanes. For years, satellites have tracked sea ice growth each winter and the dramatic extent of sea ice melt each summer. In the Arctic Ocean, thermohaline (i.e., temperature- and salt-controlled) layering is vital to maintaining the cold, relatively fresh surface waters that support diverse ecosystems. However, measuring cold-water salinity from space is challenging.

Antarctica is a large continent surrounded by the Southern Ocean. Because of this geography, sea ice has more room to expand in the winter. So, sea ice – along with other ice that originated on land such as icebergs – can move into warmer latitudes and melt. Being the only place where our seas circle Earth without being slowed down by land, the Southern Ocean is prone to very high winds. Along with cold temperatures, a wind-roughened sea surface hampers the accurate measurement of salinity from satellite.

Use the tool below – based on studies by Lind et al. (2018) and Haumann et al. (2016) – to investigate the characteristics of salinity in the Arctic and Antarctic. Use the buttons to toggle between locations.

tabs_shortcode2
Antarctic and Arctic sea ice. Credit: NASA Goddard Space Flight Center
  • Icy OceanIn the past, the Arctic Ocean was largely covered by perennial ice that lasted from year to year. Towards its outer edge – away from the North Pole – ice cover varied with the seasons.
  • Fresh Upper LayerMelt water from ice kept the upper Arctic Ocean relatively fresh. The atmosphere kept the shallow upper ocean layers very cold.
  • Warm & Salty DepthsCold, fresh upper layers had relatively low density, keeping them afloat above deeper waters. Where did the deep waters come from? The warmer, saltier and denser Atlantic Ocean.
  • Salty InterfaceThe density boundary between shallow waters and deeper waters allowed some upward flux of heat and salt.
  • Since Mid-2010'sThere has been a drastic reduction in Arctic Ocean ice cover, both year-to-year and seasonally. The warm, salty waters of the Atlantic have shifted northward.
  • AtlantificationThis term is used to describe the increased flow of Atlantic water into the Arctic. This flow decreases the depth of the shallow fresh, cold layer.
  • Fresh Water InputsBoth melting sea ice and increased outflow from rivers deliver fresh water to the Arctic Ocean. These processes have helped to balance "Atlantification" to some degree.
  • Breaking Down BarriersHowever, as Atlantic waters shift northward, there has been an increase in the upward flux of heat and salt. This weakens stratification in the Arctic Ocean.
  • Warming the AtmosphereMoreover, loss of ice cover allows warm water to directly transfer heat into the atmosphere, warming our climate.
Icy Ocean1 Fresh Upper Layer2 Warm & Salty Depths3 Salty Interface4 Since Mid-2010's5 Atlantification5 Fresh Water Inputs5 Breaking Down Barriers5 Warming the Atmosphere5
  • Icy Edge of a ContinentThe coast surrounding Antarctica has sea ice, floating ice shelves, and icebergs that have broken off the continent. Moving northward, it transitions to the open ocean.
  • Salty LayersThe ocean is layered by density. Relatively fresh waters are found near the surface with saltier layers below.
  • Sea Ice FreezingThe freezing of seawater to form sea ice moves freshwater out of the ocean, as shown by the green arrows. Salt is left behind, shown by red arrows.
  • Ice MeltingThe melting of ice moves freshwater into the ocean, shown by green arrows pointing down.
  • Northern TransportIn addition, sea ice motion away from the continent of Antarctica moves freshwater towards the north.
  • More Ice Melting and...Studies reveal how Southern Ocean salinity changed from 1982 to 2008. Melting of land ice, ice shelves, and sea ice added freshwater to the coast. This is shown by the white arrow.
  • ...Less Ice FreezingAlso, reduced formation of sea ice slowed down the movement of freshwater out of the ocean, as shown by green arrows.
  • Salinity Signals at DepthFarther away from the coast, the surface layer was freshened by increased ice melt, affecting Southern Ocean circulation.
  • Climate Change SignalsScientists have noted that "recent salinity changes in the Southern Ocean are among the most prominent signals of climate change in the global ocean." The trends depicted here may be major contributors to these changes.
Icy Edge of a Continent1 Salty Layers2 Sea Ice Freezing3 Ice Melting4 Northern Transport5 More Ice Melting and...5 ...Less Ice Freezing5 Salinity Signals at Depth5 Climate Change Signals5


tabs_shortcode2
  • Arctic Minimum (Sep 1990)

  • Arctic Minimum (Sep 1991)

  • Arctic Minimum (Sep 1992)

  • Arctic Minimum (Sep 1993)

  • Arctic Minimum (Sep 1994)

  • Arctic Minimum (Sep 1995)

  • Arctic Minimum (Sep 1996)

  • Arctic Minimum (Sep 1997)

  • Arctic Minimum (Sep 1998)

  • Arctic Minimum (Sep 1999)

  • Arctic Minimum (Sep 2000)

  • Arctic Minimum (Sep 2001)

  • Arctic Minimum (Sep 2002)

  • Arctic Minimum (Sep 2003)

  • Arctic Minimum (Sep 2004)

  • Arctic Minimum (Sep 2005)

  • Arctic Minimum (Sep 2006)

  • Arctic Minimum (Sep 2007)

  • Arctic Minimum (Sep 2008)

  • Arctic Minimum (Sep 2009)

  • Arctic Minimum (Sep 2010)

  • Arctic Minimum (Sep 2011)

  • Arctic Minimum (Sep 2012)

  • Arctic Minimum (Sep 2013)

  • Arctic Minimum (Sep 2014)

  • Arctic Minimum (Sep 2015)

  • Arctic Minimum (Sep 2016)

  • Arctic Minimum (Sep 2017)

  • Arctic Minimum (Sep 2018)

  • Arctic Minimum (Sep 2019)

  • Artic Maxima (Mar 1991)

  • Artic Maxima (Mar 1992)

  • Artic Maxima (Mar 1993)

  • Artic Maxima (Mar 1994)

  • Artic Maxima (Mar 1995)

  • Artic Maxima (Mar 1996)

  • Artic Maxima (Mar 1997)

  • Artic Maxima (Mar 1998)

  • Artic Maxima (Mar 1999)

  • Artic Maxima (Mar 2000)

  • Artic Maxima (Mar 2001)

  • Artic Maxima (Mar 2002)

  • Artic Maxima (Mar 2003)

  • Artic Maxima (Mar 2004)

  • Artic Maxima (Mar 2005)

  • Artic Maxima (Mar 2006)

  • Artic Maxima (Mar 2007)

  • Artic Maxima (Mar 2008)

  • Artic Maxima (Mar 2009)

  • Artic Maxima (Mar 2010)

  • Artic Maxima (Mar 2011)

  • Artic Maxima (Mar 2012)

  • Artic Maxima (Mar 2013)

  • Artic Maxima (Mar 2014)

  • Artic Maxima (Mar 2015)

  • Artic Maxima (Mar 2016)

  • Artic Maxima (Mar 2017)

  • Artic Maxima (Mar 2018)

  • Artic Maxima (Sep 2019)

  • Antarctic Minimum (Feb 1992)

  • Antarctic Minimum (Feb 1993)

  • Antarctic Minimum (Feb 1994)

  • Antarctic Minimum (Feb 1995)

  • Antarctic Minimum (Feb 1996)

  • Antarctic Minimum (Feb 1997)

  • Antarctic Minimum (Feb 1998)

  • Antarctic Minimum (Feb 1999)

  • Antarctic Minimum (Feb 2000)

  • Antarctic Minimum (Feb 2001)

  • Antarctic Minimum (Feb 2002)

  • Antarctic Minimum (Feb 2003)

  • Antarctic Minimum (Feb 2004)

  • Antarctic Minimum (Feb 2005)

  • Antarctic Minimum (Feb 2006)

  • Antarctic Minimum (Feb 2007)

  • Antarctic Minimum (Feb 2008)

  • Antarctic Minimum (Feb 2009)

  • Antarctic Minimum (Feb 2010)

  • Antarctic Minimum (Feb 2011)

  • Antarctic Minimum (Feb 2012)

  • Antarctic Minimum (Feb 2013)

  • Antarctic Minimum (Feb 2014)

  • Antarctic Minimum (Feb 2015)

  • Antarctic Minimum (Feb 2016)

  • Antarctic Minimum (Feb 2017)

  • Antarctic Minimum (Feb 2018)

  • Antarctic Minimum (Feb 2019)

  • Antarctic Minimum (Feb 2020)

  • Antarctic Maxima (Sep 1991)

  • Antarctic Maxima (Sep 1992)

  • Antarctic Maxima (Sep 1993)

  • Antarctic Maxima (Sep 1994)

  • Antarctic Maxima (Sep 1995)

  • Antarctic Maxima (Sep 1996)

  • Antarctic Maxima (Sep 1997)

  • Antarctic Maxima (Sep 1998)

  • Antarctic Maxima (Sep 1999)

  • Antarctic Maxima (Sep 2000)

  • Antarctic Maxima (Sep 2001)

  • Antarctic Maxima (Sep 2002)

  • Antarctic Maxima (Sep 2003)

  • Antarctic Maxima (Sep 2004)

  • Antarctic Maxima (Sep 2005)

  • Antarctic Maxima (Sep 2006)

  • Antarctic Maxima (Sep 2007)

  • Antarctic Maxima (Sep 2008)

  • Antarctic Maxima (Sep 2009)

  • Antarctic Maxima (Sep 2010)

  • Antarctic Maxima (Sep 2011)

  • Antarctic Maxima (Sep 2012)

  • Antarctic Maxima (Sep 2013)

  • Antarctic Maxima (Sep 2014)

  • Antarctic Maxima (Sep 2015)

  • Antarctic Maxima (Sep 2016)

  • Antarctic Maxima (Sep 2017)

  • Antarctic Maxima (Sep 2018)

  • Antarctic Maxima (Sep 2019)

Choose among four slideshows featuring minimum and maximum sea ice concentrations around the Arctic and Antarctica since 1990. Minima show the months of September and February for the Artic and Antarctic, respectively. Maxima shows the months of March and September, for the Arctic and Antarctic, respectively. (Source: NASA Earth Observatory's World of Change – Arctic & Antarctic)

Featured Publications

Changes in Arctic freshwater distribution impacts ocean circulation, climate, and life. This study explores the use of satellite-derived sea surface salinity (SSS) as a proxy for Arctic freshwater changes. It builds on previous work that used satellite‐derived sea surface height (SSH) and ocean bottom pressure (OBP) to infer depth‐integrated freshwater content changes. This proof‐of‐concept study analyzes the output of an ocean‐ice state estimation product, finding that SSS variations are coherent with SSH-minus-OBP across much of the Arctic basin.

Reference

Fournier, S., Lee, T., Wang, X., Armitage, T., Wang, O., Fukumori, I., and Kwok, R. (2020). Read the full paper.

Hudson Bay, the largest semi-inland sea in the Northern Hemisphere, is completely covered by ice and snow in winter. About six months each year, however, satellite remote sensing of sea surface salinity (SSS) can be retrieved over open water. This provides some insight into freshwater cycles in the Arctic Ocean where SSS data are scarce. The study found that the main source of the year-to-year SSS variability in Hudson Bay is sea ice melting. The freshwater contribution from surface forcing precipitation minus evaporation (P-E) is smaller in magnitude but lasts through the entire open water season. River discharge is comparable with P-E in magnitude but peaks before ice melt. View the one-pager.

Reference

Tang, W., Yueh, S., Yang, D., Mcleod, E., Fore, A., Hayashi, A., Olmedo, E., Martínez, J., and Gabarró, C. (2020). Read the full paper.

This study presents the first systematic analysis of six commonly used sea surface salinity (SSS) products from NASA and the European Space Agency in terms of their consistency among one another and with in-situ data. When averaged over the Arctic Ocean, the products show excellent consistency in capturing seasonal and year-to-year variations. The products also consistently identify regions with strong SSS variability over time. However, many challenges still exist in retrieving Arctic SSS because brightness temperature (TB) has lower sensitivity in colder waters at the frequency employed by today's SSS satellites (i.e., L-band). View the One-pager. Read about an evaluation and intercomparison of SMOS, Aquarius, and SMAP SSS products in our Research Insights.

Reference

Fournier, S., Lee, T., Tang, W., Steele, M., and Olmedo, E. (2019). Read the full paper.