Space climate

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Reconstruction of solar activity over 11,400 years. Period of equally high activity over 8,000 years ago marked. Sunspots 11000 years.svg
Reconstruction of solar activity over 11,400 years. Period of equally high activity over 8,000 years ago marked.

Space climate is the long-term variation in solar activity within the heliosphere, including the solar wind, the Interplanetary magnetic field (IMF), and their effects in the near-Earth environment, including the magnetosphere of Earth and the ionosphere, the upper and lower atmosphere, climate, and other related systems. The scientific study of space climate is an interdisciplinary field of space physics, solar physics, heliophysics, and geophysics. It is thus conceptually related to terrestrial climatology, and its effects on the atmosphere of Earth are considered in climate science. [1] [2] [3]

Contents

Background

Space climatology considers long-term (longer than the latitudinally variable 27-day solar rotation period, through the 11-year solar cycle and beyond, up to and exceeding millennia) variability of solar indices, cosmic ray, heliospheric parameters, and the induced geomagnetic, ionospheric, atmospheric, and climate effects. [1] It studies mechanisms and physical processes responsible for their variability in the past with projections onto future. [2] It is a broader and more general concept than space weather, to which it is related like the conventional climate and weather. [1]

In addition to real-time solar observations, the field of research also covers analysis of historical space climate data. This has included analysis and reconstruction that has allowed solar wind and heliospheric magnetic field strengths to be determined from back to 1611. [3]

Artist's rendering of Deep Space Climate Observatory (DSCOVR) DSCOVR spacecraft model.png
Artist's rendering of Deep Space Climate Observatory (DSCOVR)

The importance of space climate research has been recognized, in particular, by NASA which launched a special space mission Deep Space Climate Observatory (DSCOVR) [4] dedicated to monitoring of space climate. [5] New results, ideas and discoveries in the field of Space Climate are published in a focused peer-review research Journal of Space Weather and Space Climate (JSWSC). [6] Since 2013, research awards and medals in space weather and space climate are annually awarded by the European Space Weather Week. [7] Another recent space observatory platform is the Solar Radiation and Climate Experiment (SORCE).

Space climate research has three main aims: [1]

  1. to better understand the long-term solar variability, including also the observed extremes and features of this variability in the solar wind and in the heliospheric magnetic field
  2. to better understand the physical relationships between the Sun, the heliosphere, and various related proxies (geomagnetic fields, cosmic rays, etc.)
  3. to better understand the long-term effect of solar variability on the near-Earth environment, including the different atmospheric layers, and ultimately on Earth's global climate

History

In the early 2000s, when the concept of space weather became common, a small initiative group, led by Kalevi Mursula and Ilya G. Usoskin the University of Oulu in Finland had realized that physical drivers of solar variability and its terrestrial effects can be better understood with a more general and broader view. The concept of Space Climate had been developed, and the corresponding research community formed, which presently includes a few hundred active members around the world. In particular, a series of International Space Climate Symposia (biennial since 2004) was organized, [8] with the first inaugural symposium being held in Oulu (Finland) in 2004, followed by those in Romania (2006), Finland (2009), India (2011), Finland (2013), Finland (2016), Canada (2019), Poland (2022) and Japan (2024) as well as topical space climate sessions are regularly held at the General Assemblies of the Committee on Space Research and Earth Science. [9] [10]

Dissemination

Research results related to Space Climate are published in a bunch of peer-reviewed journals, such as Astronomy & Astrophysics, Journal of Geophysical Research, Geophysical Research Letters, Solar Physics (journal), Advances in Space Research.

See also

Related Research Articles

<span class="mw-page-title-main">Solar wind</span> Stream of charged particles from the Sun

The solar wind is a stream of charged particles released from the upper atmosphere of the Sun, called the corona. This plasma mostly consists of electrons, protons and alpha particles with kinetic energy between 0.5 and 10 keV. The composition of the solar wind plasma also includes a mixture of materials found in the solar plasma: trace amounts of heavy ions and atomic nuclei of elements such as carbon, nitrogen, oxygen, neon, magnesium, silicon, sulfur, and iron. There are also rarer traces of some other nuclei and isotopes such as phosphorus, titanium, chromium, and nickel's isotopes 58Ni, 60Ni, and 62Ni. Superimposed with the solar-wind plasma is the interplanetary magnetic field. The solar wind varies in density, temperature and speed over time and over solar latitude and longitude. Its particles can escape the Sun's gravity because of their high energy resulting from the high temperature of the corona, which in turn is a result of the coronal magnetic field. The boundary separating the corona from the solar wind is called the Alfvén surface.

<span class="mw-page-title-main">Maunder Minimum</span> Period of low solar activity, 1645–1715

The Maunder Minimum, also known as the "prolonged sunspot minimum", was a period around 1645 to 1715 during which sunspots became exceedingly rare. During a 28-year period (1672–1699) within the minimum, observations revealed fewer than 50 sunspots. This contrasts with the typical 40,000–50,000 sunspots seen in modern times over a similar timespan.

<span class="mw-page-title-main">Space weather</span> Branch of space physics and aeronomy

Space weather is a branch of space physics and aeronomy, or heliophysics, concerned with the varying conditions within the Solar System and its heliosphere. This includes the effects of the solar wind, especially on the Earth's magnetosphere, ionosphere, thermosphere, and exosphere. Though physically distinct, space weather is analogous to the terrestrial weather of Earth's atmosphere. The term "space weather" was first used in the 1950s and popularized in the 1990s. Later, it prompted research into "space climate", the large-scale and long-term patterns of space weather.

<span class="mw-page-title-main">Earth's magnetic field</span> Magnetic field that extends from the Earths outer and inner core to where it meets the solar wind

Earth's magnetic field, also known as the geomagnetic field, is the magnetic field that extends from Earth's interior out into space, where it interacts with the solar wind, a stream of charged particles emanating from the Sun. The magnetic field is generated by electric currents due to the motion of convection currents of a mixture of molten iron and nickel in Earth's outer core: these convection currents are caused by heat escaping from the core, a natural process called a geodynamo.

<span class="mw-page-title-main">Geomagnetic storm</span> Disturbance of the Earths magnetosphere

A geomagnetic storm, also known as a magnetic storm, is a temporary disturbance of the Earth's magnetosphere caused by a solar wind shock wave.

<span class="mw-page-title-main">Whistler (radio)</span> Very low frequency EM waves generated by lightning

A whistler is a very low frequency (VLF) electromagnetic (radio) wave generated by lightning. Frequencies of terrestrial whistlers are 1 kHz to 30 kHz, with maximum frequencies usually at 3 kHz to 5 kHz. Although they are electromagnetic waves, they occur at audio frequencies, and can be converted to audio using a suitable receiver. They are produced by lightning strikes where the impulse travels along the Earth's magnetic field lines from one hemisphere to the other. They undergo dispersion of several kHz due to the slower velocity of the lower frequencies through the plasma environments of the ionosphere and magnetosphere. Thus they are perceived as a descending tone which can last for a few seconds. The study of whistlers categorizes them into Pure Note, Diffuse, 2-Hop, and Echo Train types.

<span class="mw-page-title-main">Solar cycle</span> Periodic change in the Suns activity

The solar cycle, also known as the solar magnetic activity cycle, sunspot cycle, or Schwabe cycle, is a nearly periodic 11-year change in the Sun's activity measured in terms of variations in the number of observed sunspots on the Sun's surface. Over the period of a solar cycle, levels of solar radiation and ejection of solar material, the number and size of sunspots, solar flares, and coronal loops all exhibit a synchronized fluctuation from a period of minimum activity to a period of a maximum activity back to a period of minimum activity.

A solar storm is a disturbance on the Sun, which can emanate outward across the heliosphere, affecting the entire Solar System, including Earth and its magnetosphere, and is the cause of space weather in the short-term with long-term patterns comprising space climate.

<span class="mw-page-title-main">Solar Dynamics Observatory</span> NASA mission, launched in 2010 to SE-L1

The Solar Dynamics Observatory (SDO) is a NASA mission which has been observing the Sun since 2010. Launched on 11 February 2010, the observatory is part of the Living With a Star (LWS) program.

Space physics, also known as space plasma physics, is the study of naturally occurring plasmas within Earth's upper atmosphere and the rest of the Solar System. It includes the topics of aeronomy, aurorae, planetary ionospheres and magnetospheres, radiation belts, and space weather. It also encompasses the discipline of heliophysics, which studies the solar physics of the Sun, its solar wind, the coronal heating problem, solar energetic particles, and the heliosphere.

<span class="mw-page-title-main">Heliophysics</span> Science of the heliosphere

Heliophysics is the physics of the Sun and its connection with the Solar System. NASA defines heliophysics as "(1) the comprehensive new term for the science of the Sun - Solar System Connection, (2) the exploration, discovery, and understanding of Earth's space environment, and (3) the system science that unites all of the linked phenomena in the region of the cosmos influenced by a star like our Sun."

<span class="mw-page-title-main">Interplanetary magnetic field</span> Magnetic field within the Solar System

The interplanetary magnetic field (IMF), now more commonly referred to as the heliospheric magnetic field (HMF), is the component of the solar magnetic field that is dragged out from the solar corona by the solar wind flow to fill the Solar System.

Geomagnetically induced currents (GIC) are electrical currents induced at the Earth's surface by rapid changes in the geomagnetic field caused by space weather events. GICs can affect the normal operation of long electrical conductor systems such as electric transmission grids and buried pipelines. The geomagnetic disturbances which induce GICs include geomagnetic storms and substorms where the most severe disturbances occur at high geomagnetic latitudes.

<span class="mw-page-title-main">Sami Solanki</span> Astronomer

Sami Khan Solanki is director of the Max Planck Institute for Solar System Research (MPS), director of the Sun-Heliosphere Department of MPS, a scientific member of the Max Planck Society, and a Chair of the International Max Planck Research School on Physical Processes in the Solar System and Beyond at the Universities of Braunschweig and Göttingen.

The Institute of Atmospheric Physics AS CR (Czech: Ústav fyziky atmosféry Akademie věd České republiky), also designated as the IAP, is part of the Academy of Sciences of the Czech Republic (AS CR). Within the IAP research institutions are combined in order to cover the whole field of science and humanities.

<span class="mw-page-title-main">Solar particle event</span> Solar phenomenon

In solar physics, a solar particle event (SPE), also known as a solar energetic particle event or solar radiation storm, is a solar phenomenon which occurs when particles emitted by the Sun, mostly protons, become accelerated either in the Sun's atmosphere during a solar flare or in interplanetary space by a coronal mass ejection shock. Other nuclei such as helium and HZE ions may also be accelerated during the event. These particles can penetrate the Earth's magnetic field and cause partial ionization of the ionosphere. Energetic protons are a significant radiation hazard to spacecraft and astronauts.

<span class="mw-page-title-main">Heliophysics Science Division</span>

The Heliophysics Science Division of the Goddard Space Flight Center (NASA) conducts research on the Sun, its extended Solar System environment, and interactions of Earth, other planets, small bodies, and interstellar gas with the heliosphere. Division research also encompasses geospace—Earth's uppermost atmosphere, the ionosphere, and the magnetosphere—and the changing environmental conditions throughout the coupled heliosphere.

<span class="mw-page-title-main">Solar phenomena</span> Natural phenomena within the Suns atmosphere

Solar phenomena are natural phenomena which occur within the atmosphere of the Sun. They take many forms, including solar wind, radio wave flux, solar flares, coronal mass ejections, coronal heating and sunspots.

<span class="mw-page-title-main">Nancy Crooker</span> American astrophysicist

Nancy U. Crooker is an American physicist and professor emerita of space physics at Boston University, Massachusetts. She has made major contributions to the understanding of geomagnetism in the Earth's magnetosphere and the heliosphere, particularly through the study of interplanetary electrons and magnetic reconnection.

<span class="mw-page-title-main">Ilya G. Usoskin</span> Finnish Astrophysicist

Ilya G. Usoskin is a Finnish astrophysicist who is a professor at University of Oulu and head of Cosmic Ray Station at Sodankylä Geophysical Observatory. He is a Vice president of the International Astronomical Union since 2021.

References

  1. 1 2 3 4 Mursula, K.; Usoskin, I.G.; Maris, G. (January 2007). "Introduction to Space Climate" (PDF). Advances in Space Research. 40 (7): 885–887. Bibcode:2007AdSpR..40..885M. doi:10.1016/j.asr.2007.07.046. ISSN   0273-1177.
  2. 1 2 González Hernández, I.; Komm, R.; Pevstsov, A.; Leibacher, J (2014). "Solar Origins of Space Weather and Space Climate: Preface". Solar Physics. 289 (2): 437–439. Bibcode:2014SoPh..289..437G. doi: 10.1007/s11207-013-0454-x .
  3. 1 2 Lockwood, M.; et al. (2017). "Space climate and space weather over the past 400 years: 1. The power input to the magnetosphere". J. Space Weather Space Climate. 7: A25. arXiv: 1708.04904 . Bibcode:2017JSWSC...7A..25L. doi:10.1051/swsc/2017019. S2CID   37433045.
  4. "DSCOVR: Deep Space Climate Observatory". NOAA . Retrieved 29 December 2018.
  5. "Space Climate Observatory Homepage". SCO. Retrieved 29 December 2018.
  6. "Journal of Space Weather and Space Climate – homepage". SWSC. Retrieved 29 December 2018.
  7. "European Space Weather Week Medals". STCE. Retrieved 29 December 2018.
  8. "Space Climate Symposia" . Retrieved 29 December 2018.
  9. Corrado Ruscica (1 August 2014). "40° Cospar Scientific Assembly". astronomicamens. Retrieved 30 December 2018.
  10. "42nd COSPAR Scientific Assembly: Nanosatellites and Space Climate Observatory share centre stage". Office for Science & Technology of the Embassy of France in the United States. 16 July 2018. Retrieved 30 December 2018.