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Walter Heinrich Munk (October 19, 1917 – February 8, 2019) was an American physical oceanographer.[1][6] He was a professor of geophysics at the Scripps Institution of Oceanography at the University of California, San Diego in La Jolla. Born to a prominent Austrian family, in 1932 Munk was sent to school in the United States at age 14. Abandoning a New York banking career, Munk obtained a scientific education at the California Institute of Technology and his doctorate from Scripps. During World War II, Munk and his doctoral advisor Harald Sverdrup developed methods for predicting surf conditions on beaches, saving countless lives during allied landings in North Africa, the Pacific, and Northern Europe. After the war, Scripps grew from a small biological station to a major research institution. Munk and his wife Judy were active in developing the Scripps campus and integrating it with the new University of California, San Diego. One of the first to bring statistical methods to the analysis of oceanographic data, Munk's work is noted for creating fruitful areas of research that continue to be explored. These areas include surface waves, geophysical implications of variations in the Earth's rotation, tides, internal waves, deep-ocean drilling into the sea floor, acoustical measurements of ocean properties, sea level rise, and climate change. In a 1991 experiment, Munk and his collaborators tested the ability of underwater sound to propagate from the Southern Indian Ocean across all ocean basins. The aim was to use the acoustic signals to measure changes in broad-scale ocean temperatures. The experiment was criticized by environmental groups, who expected that the loud acoustic signals would adversely affect marine life. Munk was a member of the JASON think tank, and he held a Secretary of the Navy/Chief of Naval Operations Oceanography Chair. Munk died at age 101 in La Jolla, California.[1]

Walter Munk
Crafoordprize 2010-03.jpg
Munk in Stockholm in 2010 to accept his Crafoord Prize.
Walter Heinrich Munk

(1917-10-19)October 19, 1917
DiedFebruary 8, 2019(2019-02-08) (aged 101)[1][2][3][4]
Alma materCalifornia Institute of Technology (BS,MS)
Scripps Institution of Oceanography/University of California, Los Angeles (PhD)
AwardsMaurice Ewing Medal (1976)
Alexander Agassiz Medal (1976)
National Medal of Science (1985)
Bakerian Lecture (1986)
William Bowie Medal (1989)
Vetlesen Prize (1993)
Kyoto Prize (1999)
Prince Albert I Medal (2001)
Crafoord Prize (2010)
Scientific career
FieldsOceanography, geophysics
ThesisIncrease in the period of waves traveling over large distances : with applications to tsunamis, swell, and seismic surface waves (1946) [5]
Doctoral advisorHarald Ulrik Sverdrup
Doctoral studentsCharles Shipley Cox


Early life and educationEdit

Munk was born in 1917 in Vienna, Austria-Hungary, to a Jewish family.[7] His father, Dr. Hans Munk, and his mother, Rega Brunner, divorced when Munk was ten years old.[8] His maternal grandfather was a prominent banker and Austrian politician, Lucian Brunner (1850–1914). His stepfather, Dr. Rudolf Engelsberg, was head of the salt mine monopoly of the Austrian government. He was therefore a member of the Austrian governments of first Chancellor Engelbert Dollfuss (assassinated by Nazis in 1934) and then Chancellor Kurt Schuschnigg (resigned after Nazi Germany annexed Austria, the Anschluss, in 1938).[8][9][10]

In 1932, Munk was performing poorly in school, because he was spending too much time skiing. So, his family sent him to a boys' preparatory school in upper New York state.[11][8] His family envisioned a career for Munk in finance with a New York bank connected to the family business. Munk worked at the family's banking firm for three years and studied at Columbia University.

Munk hated banking, however, and in 1937 he left the firm to attend the California Institute of Technology (Caltech) in Pasadena.[8] While at Caltech, he took a summer job in 1939 at the Scripps Institution of Oceanography (Scripps) in La Jolla, California.[9] Munk earned a B.S. in applied physics in 1939[11] and an M.S. in geophysics in 1940 at Caltech.[8][12] Though the M.S. degree was from Caltech, the work was based on oceanographic data collected in the Gulf of California by the Norwegian oceanographer Harald Sverdrup.[10] Sverdrup, the director of Scripps, was the thesis advisor.

In 1939, Munk asked Sverdrup to take him on as a doctoral student. Sverdrup agreed, but told Munk that he did "not know of a single job in oceanography which would become available in the next decade".[8] However, Munk's studies were interrupted by the outbreak of World War II. He completed his doctoral degree in oceanography at Scripps under the University of California, Los Angeles in 1947.[5][8]

Personal lifeEdit

Munk applied to be a citizen of the United States in 1938, but he failed the citizenship test by giving an overly-detailed answer to a question about the Constitution.[8] Munk obtained American citizenship in 1939.

Munk married Martha Chapin in the late 1940s. The marriage ended in divorce in 1953.[8]

On June 20, 1953, Munk married Judith Horton. She was an active participant at Scripps for decades, where she made contributions to architecture, campus planning, and the renovation and reuse of historical buildings. The Munks were frequent traveling companions. Judith Munk died in 2006.[13]

Munk married La Jolla community leader Mary Coakley in June 2011.[13]

Munk turned 100 in October 2017.[14] He died of pneumonia on February 8, 2019 at La Jolla, California, aged 101.[1][15]

Wartime activitiesEdit

After the Anschluss, Munk enlisted in the ski troops of the U.S. Army as a private in 1940. Enlistment in the Army was unusual, as all the other young men at Scripps joined the U.S. Naval Reserve.[16] At the request of Sverdrup and Roger Revelle, Munk was discharged from military service to undertake defense-related research at Scripps. His discharge was in December 1941, a week before the Japanese Attack on Pearl Harbor.[8] He joined several of his colleagues from Scripps at the U.S. Navy Radio and Sound Laboratory, where they developed methods related to antisubmarine and amphibious warfare.

Predicting surf conditions for Allied landingsEdit

In 1943, Munk and Sverdrup began working on the problem of predicting heights of ocean surface waves. Munk had observed troops in practice beach landings in the Carolinas and noted that waves larger than about five feet were dangerous to people and landing craft.[8] The methods they developed to predict surf conditions were used during Allied landings in North Africa, the Pacific theater of war, and on D-Day during the Normandy invasion.[9][17] Countless lives were saved by these predictions. Munk commented in 2009:[18]

The Normandy landing is famous because weather conditions were very poor and you may not realize it was postponed by General Eisenhower for 24 hours because of the prevailing wave conditions. And then he did decide, in spite of the fact that conditions were not favorable, it would be better to go in than lose the surprise element, which would have been lost if they waited for the next tidal cycle [in] two weeks.

Oceanographic measurements during atomic weapons tests in the PacificEdit

In 1946, the United States tested two fission nuclear weapons (20 kilotons) at Bikini Atoll in the equatorial Pacific in Operation Crossroads. Munk helped to determine the currents, diffusion, and water exchanges affecting the radiation contamination from the second test, code-named Baker.[9][7] Munk returned to the equatorial Pacific six years later to Eniwetok Atoll, for the 1952 test of the first fusion nuclear weapon (10 megatons), code-named Ivy Mike.[8] Roger Revelle, John Isaacs, and Munk had initiated a program for monitoring for the possibility of a large tsunami generated from the test.[8]

The Institute of Geophysics and Planetary Physics in La JollaEdit

After receiving his doctorate in 1947, Munk was hired by Scripps as an assistant professor of geophysics. He became a full professor there in 1954.[19]

In 1955, Munk took a sabbatical at Cambridge University in England with a Guggenheim Fellowship.[8] Returning to Scripps in 1956, Munk developed plans for a La Jolla branch of the Institute of Geophysics (IGP). IGP was an institution of the University of California system, and Munk's faculty appointment was at its Los Angeles campus. With the new branch to be focused on planetary physics with an emphasis on the Earth-Moon system, IGP changed its name to the Institute of Geophysics and Planetary Physics (IGPP). IGPP at La Jolla was built between 1959–1963 with funding from the University of California, the U.S. Air Force Office of Scientific Research, the National Science Foundation, and private foundations.[20][21] The redwood building was designed by architect Lloyd Ruocco, in close consultation with Judith and Walter Munk. The IGPP buildings have become the center of the Scripps campus. Among the early faculty appointments were Carl Eckart, George Backus, Freeman Gilbert and John Miles. The eminent geophysicist Sir Edward "Teddy" Bullard was a regular visitor to IGPP. In 1971 an endowment of $600,000 was established by Cecil Green to support visiting scholars, now known as Green Scholars. Munk served as director of IGPP/LJ from 1962–1982.[20][8]

As an academic institution, from 1938 until 1958 Scripps was under the administration of the University of California, Los Angeles. Scripps became part of the University of California, San Diego when it was formed in 1958.[22] Roger Revelle, then director of Scripps, was a primary advocate for establishing the La Jolla campus.[23]

In the late 1980s, plans for an expansion of IGPP were developed by Judith and Walter Munk, and Sharyn and John Orcutt, in consultation with a local architect, Fred Liebhardt.[20] The Revelle Laboratory was completed in 1993. At this time the original IGPP building was renamed the Walter and Judith Munk Laboratory for Geophysics. In 1994 the Scripps branch of IGPP was renamed the Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics.[20]

Career ActivitiesEdit

In 1968, Munk became a member of JASON, a panel of scientists who advise the U.S. government.[24]

In 1981, Munk became a founding member of the World Cultural Council.[25]

Munk held a Secretary of the Navy/Chief of Naval Operations Oceanography Chair from 1985 until his death in 2019.[8]


Munk's career in oceanography and geophysics touched on disparate and innovative topics. A pattern of Munk's work was that he would initiate a completely new topic, ask challenging, fundamental questions about the subject and its larger meaning, then, having created an entirely new sub-field of science, move on to another new topic.[1][26] As Carl Wunsch, one of Munk's frequent collaborators,[27] commented:[8]

[Walter has] a sometimes uncanny ability to delineate the essence - that had eluded his predecessors - of a central problem. He has the knack of defining a field in a way that requires decades of subsequent work by others to fully flesh-out, while he himself moves on. One of his explicitly stated themes is that it is more important to ask the right questions than it is to give the right answers.

The five major ocean gyres

Wind-driven gyresEdit

In 1948, Munk took a year's sabbatical to visit Sverdrup in Oslo, Norway on his first Guggenheim Fellowship.[16] He worked on the problem of wind-driven ocean circulation.[8] Munk's pioneering research, published in 1950, shows that Gulf Stream transport can be estimated by integrating the wind stress across the Atlantic.[28] Munk coined the term "wind-driven gyres," a term now widely used.[8]

Rotation of the EarthEdit

In the 1950s, Munk investigated irregularities in the Earth's rotation, such as the Chandler wobble and annual and long-term changes in the length of day (rate of the Earth's rotation). These small variations are related to geophysical processes, such as the changes in the atmosphere, ocean, and core, and the energy dissipated by tidal acceleration. He also investigated how western boundary currents, such as the Gulf Stream, dissipated planetary vorticity. Munk thoroughly reviewed and explored the subject in the 1960 monograph, written with G.J.F. MacDonald, The Rotation of the Earth: A Geophysical Discussion. The discussion is written from a geophysical, rather than astronomical, perspective, in particular, the monograph emphasizes using variation in the Earth's rotation to infer geophysical properties. The monograph is a standard reference.[29][30]

Project Mohole contracted with a consortium of oil companies use of their oil drillship CUSS I to drill into the sea floor in deep water.[31]

Project MoholeEdit

In 1957, Munk and Harry Hess suggested the idea behind Project Mohole: to drill into the Mohorovicic Discontinuity and obtain a sample of the Earth's mantle. While such a project was not feasible on land, drilling in the open ocean would be more feasible, because the mantle is much closer to the sea floor. Initially led by the informal group of scientists known as the American Miscellaneous Society (AMSOC, including Hess, Maurice Ewing, and Roger Revelle),[8] the project was eventually taken over by the National Science Foundation (NSF). Initial test drillings into the sea floor led by Willard Bascom occurred off Guadalupe Island, Mexico in March and April 1961.[32] The project was mismanaged and grew in expense after the construction company Brown and Root won the contract to continue the effort, however, and Congress discontinued the project toward the end of 1966.[33] While Project Mohole was not successful, the idea led to projects such as NSF's Deep Sea Drilling Program.[34]

Ocean swellEdit

Munk conducted groundbreaking research on R/P FLIP's first science mission, leading to an increased understanding of waves traveling across ocean basins.[35]

Starting in the late 1950s, Munk returned to the study of ocean waves. Thanks to his acquaintance with John Tukey, he pioneered the use of power spectra in describing wave behavior. This work culminated with an expedition that he led in 1963 called "Waves Across the Pacific" to observe waves generated by storms in the Southern Indian Ocean. Such waves traveled northward for thousands of miles across the Pacific Ocean. To trace the path and decay of the waves, he established measurement stations on islands and at sea (on R/P FLIP) along a great circle from New Zealand, to the Palmyra Atoll, and finally to Alaska.[36] Munk and his family spent nearly the whole of 1963 on American Samoa for this experiment. Walter and Judith Munk collaborated in making a film to document the experiment.[37] The results show little decay of wave energy with distance traveled.[38] This work, together with the wartime work on wave forecasting, led to the science of surf forecasting, one of Munk's best-known accomplishments.[18] Munk's pioneering research into surf forecasting was acknowledged in 2007 with an award from the Groundswell Society, a surfing advocacy organization.[39][40]

Ocean tidesEdit

Between 1965 and 1975, Munk turned to investigations of ocean tides, partially motivated by their effects on the Earth's rotation. Modern methods of time-series and spectral analysis were brought to bear on tidal analysis, leading to the development of the "response method" of tidal analysis.[41] With Frank Snodgrass, Munk developed deep-ocean pressure sensors that could be used to provide tidal data far from any land.[11][42] One highlight of this work was the discovery of the semidiurnal amphidrome midway between California and Hawaii.[43]

Internal waves: The Garrett-Munk SpectrumEdit

At the time of Munk's dissertation for his master's degree in 1939, internal waves were considered to be an uncommon phenomenon.[8] By the 1970s, there were extensive published observations of internal-wave variability in the oceans in temperature, salinity, and velocity as functions of time, horizontal distance, and depth. Motivated by a 1958 paper by Owen Philips that described a universal spectral form for the variance of ocean surface waves as a function of wave number,[11] Chris Garrett and Munk attempted to make sense of the observations by postulating a universal spectrum for internal waves.[44] According to Munk,[8] they chose a spectrum that could be factored into a function of frequency times a function of vertical wave number. The resulting spectrum, now called the Garrett-Munk Spectrum, is roughly consistent with a large number of diverse measurements that had been obtained over the global ocean. The model evolved over the subsequent decade, denoted GM72, GM75, GM79, etc.,[45] according to the year of publication of the revised model. Although Munk expected the model to be rapidly obsolete, it proved to be a universal model that is still in use. Its universality is interpreted as indicating profound processes governing internal wave dynamics, turbulence and fine-scale mixing.[11] Klaus Hasselmann commented in 2010, "...the publication of the GM spectrum has indeed been extremely fruitful for oceanography, both in the past and still today."[8]

Ocean acoustic tomographyEdit

During the 1991 Heard Island Feasibility Test (HIFT), acoustic signals were transmitted from the MV Cory Chouest steaming near Heard Island in the Southern Indian Ocean. The signals followed geodesic paths to receivers located throughout the world oceans. The experiment tested the ability of sound to measure the temperatures of the major ocean basins.

Beginning in 1975, Munk and Carl Wunsch of the Massachusetts Institute of Technology pioneered the development of acoustic tomography of the ocean.[46] With Peter Worcester and Robert Spindel,[26] Munk developed the use of sound propagation, particularly sound arrival patterns and travel times, to infer important information about the ocean's large-scale temperature and current. This work, together with the work of other groups,[47] eventually motivated the 1991 "Heard Island Feasibility Test" (HIFT), to determine if man-made acoustic signals could be transmitted over antipodal distances to measure the ocean's climate. The experiment came to be called "the sound heard around the world." During six days in January 1991, acoustic signals were transmitted by sound sources lowered from the M/V Cory Chouest near Heard Island in the southern Indian Ocean. These signals traveled half-way around the globe to be received on the east and west coasts of the United States, as well as at many other stations around the world.[48] The follow-up to this experiment was the 1996–2006 Acoustic Thermometry of Ocean Climate (ATOC) project in the North Pacific Ocean.[6][49][50] Both HIFT and ATOC engendered considerable public controversy concerning the possible effects of man-made sounds on marine mammals.[51][52][53][6]

Tomography has come to be a valuable method of ocean observation,[54] exploiting the characteristics of long-range acoustic propagation to obtain synoptic measurements of average ocean temperature or current. Applications have included the measurement of deep-water formation in the Greenland Sea in 1989,[55] measurement of ocean tides,[56][57] and the estimation of ocean mesoscale dynamics by combining tomography, satellite altimetry, and in situ data with ocean dynamical models.[58] In addition to the decade-long measurements obtained in the North Pacific, acoustic thermometry has been employed to measure temperature changes of the upper layers of the Arctic Ocean basins,[59] which continues to be an area of active interest.[60] Acoustic thermometry has also been used to determine changes to global-scale ocean temperatures using data from acoustic pulses traveling from Australia to Bermuda.[61][62]

Tides and mixingEdit

In the 1990s, Munk returned to the work on the role of tides in producing mixing in the ocean.[63] In a 1966 paper "Abyssal Recipes", Munk was one of the first to assess quantitatively the rate of mixing in the abyssal ocean in maintaining oceanic stratification.[64] At that time, the tidal energy available for mixing was thought to occur by processes near ocean boundaries. According to Sandström's theorem (1908), without the occurrence deep mixing, driven by, e.g., internal tides or tidally-driven turbulence in shallow regions, most of the ocean would become cold and stagnant, capped by a thin, warm surface layer.[65] The question of tidal energy available for mixing was reawakened in the 1990s with the discovery, by acoustic tomography and satellite altimetry, of large-scale internal tides radiating energy away from the Hawaiian Ridge into the interior of the North Pacific Ocean.[66][67] Munk recognized that the tidal energy from the scattering and radiation of large-scale internal waves from mid-ocean ridges was significant, hence it could drive abyssal mixing.[68]

Munk's enigmaEdit

In his later work, Munk focused on the relation between changes in ocean temperature, sea level, and the transfer of mass between continental ice and the ocean.[69][70] This work described what came to be known as "Munk's enigma", a large discrepancy between observed rate of sea level rise and its expected effects on the earth's rotation.[71][72][73]


Carl XVI Gustaf of Sweden presents the Crafoord Prize to Munk

Munk was elected to the National Academy of Sciences in 1956 and to the Royal Society of London in 1976. He was both a Guggenheim Fellow (1948, 1953, 1962)[74] and a Fulbright Fellow. He was named California Scientist of the Year by the California Museum of Science and Industry in 1969. Munk gave the 1986 Bakerian Lecture at the Royal Society on Ships from Space (paper)[75] and Acoustic monitoring of ocean gyres (lecture).[76][77][78] In July 2018 at the age of 100, Munk was appointed a Chevalier of France's Legion of Honour in recognition of his contributions to oceanography.[4]

Among the many other awards and honors Munk received are the Arthur L. Day Medal of the Geological Society of America in 1965, the Sverdrup Gold Medal of the American Meteorological Society in 1966, the Gold Medal of the Royal Astronomical Society in 1968, the first Maurice Ewing Medal of the American Geophysical Union and the U.S. Navy in 1976, the Alexander Agassiz Medal of the National Academy of Sciences in 1976, the Captain Robert Dexter Conrad Award of the U.S. Navy in 1978, the National Medal of Science in 1983, the William Bowie Medal of the American Geophysical Union in 1989, the Vetlesen Prize in 1993, the Kyoto Prize in 1999, the first Prince Albert I Medal in 2001, and the Crafoord Prize of the Royal Swedish Academy of Sciences in 2010 "for his pioneering and fundamental contributions to our understanding of ocean circulation, tides and waves, and their role in the Earth's dynamics".

In 1993, Munk was the first recipient of the Walter Munk Award given "in Recognition of Distinguished Research in Oceanography Related to Sound and the Sea."[79] This award is given jointly by the Oceanography Society, the Office of Naval Research and the US Department of Defense Naval Oceanographic Office.[79]


  • W. Munk and G.J.F. MacDonald, The Rotation of the Earth: A Geophysical Discussion, Cambridge University Press, 1960, revised 1975. ISBN 0-521-20778-9
  • W. Munk, P. Worcester, and C. Wunsch, Ocean Acoustic Tomography, Cambridge University Press, 1995. ISBN 0-521-47095-1
  • S. Flatté (ed.), R. Dashen, W. H. Munk, K. M. Watson, and F. Zachariasen, Sound Transmission through a Fluctuating Ocean, Cambridge University Press, 1979. ISBN 978-0-521-21940-2
  • H. von Storch and K. Hasselmann, Seventy Years of Exploration in Oceanography: A Prolonged Weekend Discussion with Walter Munk, Springer, 2010. ISBN 978-3-642-12086-2



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  7. ^ a b Galbraith, Kate (August 24, 2015). "Walter Munk, the 'Einstein of the Oceans'". The New York Times. Retrieved February 10, 2019.
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  21. ^ "The Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics (IGPP)". Retrieved November 2, 2010.
  22. ^ Stadtman, Verne A. (1970). The University of California, 1868-1968. McGraw-Hill. pp. 407–411. Retrieved May 5, 2013.
  23. ^ Munk, W. (1997). "Tribute to Roger Revelle and his contribution to studies of carbon dioxide and climate change". Proceedings of the National Academy of Sciences of the United States of America. 94 (16): 8275–8279. doi:10.1073/pnas.94.16.8275.
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  25. ^ "About Us". World Cultural Council. Retrieved November 8, 2016.
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  28. ^ Munk, W. (1950). "On the wind-driven ocean circulation". Journal of Meteorology. 7: 79–93.
  29. ^ Groves, G.W. (1961). "Dynamics of the Earth-Moon System". In Kopal, Z. Physics and Astronomy of the Moon. New York: Academic Press. pp. 61–98.
  30. ^ Lambeck, K.; Cazenave, A. (1977). "The Earth's variable rate of rotation: A discussion of some meteorological and oceanic causes and consequences". Phil. Trans. Roy. Soc. A. 284 (1326): 495–506. Bibcode:1977RSPTA.284..495L. doi:10.1098/rsta.1977.0025.
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