Weekly Ocean News

26-30 November 2018


Items of Interest:

Ocean in the News:

  • Australian tropical cyclone season outlook issued -- Forecasters at the Australian Government's Bureau of Meteorology recently released an outlook for the upcoming 2018-19 Australian tropical cyclone season that typically begins in November and runs through April. These forecasters foresee a fewer number of tropical cyclones than average within each of the five regions that surround the continent. They base their outlook upon the status of ENSO over the preceding July to September, the sea surface temperatures in the tropical Pacific Ocean and a survey of the suite of international outlook models. Therefore, their outlook for a lower than average tropical cyclone season is based upon the possible development of El Niño in the tropical Pacific Ocean and near average ocean temperatures to the north and east of Australia. [Australian Bureau of Meteorology]
  • Review of October 2018 global temperatures and sea ice cover -- Preliminary data analyzed by scientists at NOAA's National Centers for Environmental Information (NCEI) indicated that the global combined land and ocean average surface temperature for October 2018 was 1.55 Fahrenheit degrees above the 20th century average (1901-2000) for the month. Therefore, last month's global combined temperature was the second highest October temperature since global temperature records began in 1880, trailing the record highest October global combined temperature that was set in 2015 by 0.23 Fahrenheit degrees. When considered separately, the monthly average temperature over the global oceans for October 2018 was 1.30 Fahrenheit degrees above average. The monthly average October temperature of the land surface was 2.23 Fahrenheit degrees above average. Thus, the October 2018 temperatures over both the ocean and land surfaces ranked second in their respective records behind the record warm October 2015.
    When considering the combined land-ocean global temperature for the year to date (January-October 2018), this ten-month temperature was the fourth highest global temperature for the first ten months of any year since 1880. [NOAA/NCEI State of the Climate]
    A global map of Selected Significant Climate Anomalies and Events for October 2017 is available from NCEI.
    According to satellite data collected by National Snow and Ice Data Center, the sea ice over the Arctic Ocean during October 2018 was the third smallest areal extent for any October since satellite-derived ice records began in 1979. The sea ice around Antarctica also was the fourth smallest October ice extent in the last 40 years.
    The snow cover extent across North America in October 2018 was the second largest extent for October in 51 years of record. [NOAA/NCEI Global Snow & Ice]
  • An international global greenhouse gas information system is advanced -- Two weeks ago, the World Meteorological Organization (WMO) hosted the first symposium and user summit of the Integrated Global Greenhouse Gas Information System (IG3IS) in Geneva, Switzerland. The aim of this three-day symposium was to bring together technical developers and key users from several different sectors to help inform and guide reductions in emissions of carbon dioxide and other heat trapping greenhouse gases driving climate change. IG3IS will help support the Paris Agreement on climate change. [World Meteorological Organization Media Centre News]
  • Atmospheric greenhouse gas concentrations reach new record levels in 2017 -- The World Meteorological Organization (WMO) recently released its "WMO Greenhouse Gas Bulletin No. 14: The State of Greenhouse Gases in the Atmosphere Based on Global Observations through 2017." This report describes the state of the heat-absorbing atmospheric greenhouse gases for carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) based upon global observations through 2017. Carbon dioxide levels reached 405.5 parts per million (ppm) in 2017, a level not seen in 3-5 million years. In addition, concentrations of methane and nitrous oxide also rose, along with a resurgence of a potent greenhouse gas and ozone depleting substance called CFC-11, which is regulated under the Montreal Protocol. WMO foresees no sign of a reversal in these trends, which are driving long-term climate change, sea level rise, ocean acidification and more extreme weather. [World Meteorological Organization Media Centre]
  • United Nations climate change conference to convene -- The twenty-fourth session of the Conference of the Parties (COP 24) and the fourteenth session of the Conference of the Parties serving as the meeting of the Parties to the Kyoto Protocol (CMP 14) is set to convene next Sunday (2 December 2018) in Katowice, Poland and run through Friday, 14 December. The key objective of this Katowice Climate Change Conference is to adopt the implementation guidelines of the Paris Climate Change Agreement, namely to hold the global average temperature to as close as possible to 1.5 degrees Celsius. [United Nations Framework Convention on Climate Change COP 24]
  • Podcast provides information on harmful algal blooms -- NOAA's National Ocean Service recently posted a 15:20-minute NOAA Ocean Podcast entitled "All About HABs: Uncovering the Mystery of Harmful Algal Blooms" that features an interview with a oceanographer with the National Centers for Coastal Ocean Science who is at the NOAA Lab in Beaufort, NC. He dispels the use of the term "red tide" to identify all harmful algal blooms (HABs) and provides information on the various HABs, including how to recognize these blooms, where they occur and how they can be prevented. [NOAA National Ocean Service Podcast]
  • An ENSO conference is held in Ecuador -- A staff member at NOAA's Climate Prediction Center recently posted a blog on the ClimateWatch Magazine describing her experiences attending the IV International Conference on El Niño Southern Oscillation (ENSO) during mid-October in Guayaquil, Ecuador along with approximately 130 scientists from around the world. She discussed some topics presented at the conference, including ENSO in a warmer climate; the reasons for ENSO complexity; and the difficulties in predicting ENSO. [NOAA Climate.gov News]
  • An All-Hazards Monitor -- This Web portal provides the user information from NOAA's National Weather Service, FAA and FEMA on current environmental events that may pose as hazards such as tropical weather, fire weather, marine weather, severe weather, drought and floods. [NOAA/NWS Daily Briefing]
  • Earthweek -- Diary of the Planet [earthweek.com].

  • Concept of the Week: Climate Feedback Processes

    Earth's climate system includes many interacting variables. Some variables are external to the Earth-atmosphere system and some are internal. External variables include solar energy output and Earth-sun geometry (i.e., the Milankovitch cycles). Internal variables include properties of the Earth's surface (e.g., albedo, moisture), the concentration of key atmospheric components (e.g., greenhouse gases, sulfurous aerosols), and cloud cover and thickness.

    An important consideration in understanding how Earth's climate system responds to some perturbation is feedback. Feedback is defined as a sequence of interactions among variables in a system that determines how the system responds to some initial perturbation in one or more of the variables. Variables in Earth's climate system may interact in such a way as to either amplify (positive feedback) or lessen (negative feedback) a change in climate. An example of positive feedback is the ice-albedo effect described in Chapter 12 of the AMS Ocean Studies textbook. Less ice cover in the Arctic greatly reduces the albedo of the Arctic Ocean causing higher sea surface temperatures and accelerated melting of the multiyear pack ice.

    Consider an example of negative feedback. Increasing concentrations of atmospheric carbon dioxide enhances the greenhouse effect causing global warming. Global warming in turn raises sea surface temperatures and increases the rate of evaporation. A more humid atmosphere means more persistent and thicker cloud cover but clouds have both a cooling and warming effect on the lower atmosphere. The relatively high albedo of cloud tops causes cooling whereas absorption and emission of infrared radiation by clouds causes warming by contributing to the greenhouse effect. Satellite measurements and numerical models indicate that cooling would dominate.

    In general, negative feedback tends to dominate over positive feedback in Earth's climate system, limiting the magnitude of climate change. The great thermal inertia of the ocean is the principal reason for dampening the planetary temperature response.


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    Prepared by AMS Ocean Central Staff and Edward J. Hopkins, Ph.D., email hopkins@aos.wisc.edu
    © Copyright, 2018, The American Meteorological Society.