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Page 1: Synoptic–Dynamic meteorology and weather analysis and forecasting: a tribute to Fred Sanders, edited by Lance F. Bosart and Howard B. Bluestein. Meteorological Monograph Vol. 33

QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETYQ. J. R. Meteorol. Soc. 135: 1914–1915 (2009)Published online in Wiley InterScience(www.interscience.wiley.com) DOI: 10.1002/qj.507

BOOK REVIEW

SYNOPTIC–DYNAMIC METEOROLOGY ANDWEATHER ANALYSIS AND FORECASTING: ATRIBUTE TO FRED SANDERS, edited by LanceF. Bosart and Howard B. Bluestein. MeteorologicalMonograph Vol. 33 No. 55, American Meteorologi-cal Society, 2008. Hardcover, $120, 440 pp. ISBN978-1-878220-84-4

Fred Sanders (1923–2006), Emeritus Professor ofMeteorology at the Massachusetts Institute of Technol-ogy, was a leading light in synoptic meteorology fordecades. His teaching inspired several generations of stu-dents. The great respect he commanded shines throughthe pages of this book, written by many of his formerstudents and collaborators. The book illustrates the evo-lution of our understanding of the atmosphere over thepast half century, and is a valuable record of the majorcontributions of Sanders, in whose honour this collectionof articles has been assembled.

The scientific rigour of synoptic meteorology has beenquestioned from time to time. Fred Sanders provideda solid scientific foundation for his synoptic studies bymerging the application of dynamics and quantitativediagnosis with his studies of observed weather systems.Sanders believed in using time series of conventional sur-face observations for all that they are worth, extractingfrom them maximum understanding of how the funda-mental dynamical principles manifest themselves in syn-optic developments.

The book is a collection of sixteen articles, generally byleading figures in synoptic or dynamic meteorology. It isheavily American in content, with almost all the twenty-eight authors coming from the USA, and the synopticcases have an emphasis on the Southern Plains and EastCoast of the United States. The book is in four parts, withIntroductions to Parts 1 and 2 by Howard Bluestein, andto Parts 3 and 4 by Lance Bosart.

Part 1, on Fronts, has six chapters, the first (Bluestein)on surfaces of discontinuity and their role in the initiationof convective storms. This is followed by a chapter onfronts in sloping terrain (Bosart, Wasula, Drag, Meier).Then comes a discussion of the out-of-date conceptof air masses (Emanuel), with a proposal for a newdefinition in terms of saturation potential temperature.Next is an empirical perspective on cold fronts (Kessler)illustrating some limitations of the Norwegian model.This reflects one of Sanders’ concerns: ‘What I dosee wrong is the practice of identifying ALL windshifts, whether accompanied or not by density contrast,as fronts’. The critical role of surface observations insynoptic analysis is stressed here once again. Chapter5 (Schultz) provides an excellent review of the highs

and lows of fashion of frontal theory, and of Sanders’work in shaping the role of frontal theory in synopticanalysis. The author discusses the complexity of realfronts, revisiting Sanders’ observation that when thewind shift is coincident with the temperature gradient,frontogenesis ensues; when the wind shift or pressuretrough lies ahead, frontolysis results. In the final chapterof Part 1 (Schultz and Roebber), the front analysedin Sanders’ seminal 1955 paper is simulated with amesoscale NWP model, MM5. Methods hardly imaginedfifty years ago shine new light on Sanders’ study, showingsome weaknesses, but also the remarkable strengths of hisoriginal analysis.

Part 2 comprises four chapters on Analysis and Diag-nosis. The first (Hakim and Torn) describes techniquesavailable for ensemble synoptic analysis and demon-strates them by illustrative examples. The next (Hoff-man) discusses the use of surface potential temperatureanalysis and its capacity to distinguish between fronts,baroclinic troughs and non-frontal baroclinic zones. Thethird (Nielsen-Gammon and Gold) expounds the view thatPV (potential vorticity) thinking, which is consistent withcommonly used QG (quasi-geostrophic) diagnostic tech-niques, is overdue in the United States. The conclusionis that PV ‘helps the forecaster see what the atmosphereis capable of doing, thereby helping not just the forecastitself but also the forecast of what can go wrong’, i.e.forecast uncertainty. Part 2 ends with an article (Weiss,Bluestein, Pazmany and Geerts) on a fine-scale radaranalysis of a dry-line, in which the authors present obser-vational evidence of vertical velocities up to 10 m/s at500 m.

Part 3 comprises four articles on forecasting. Thefirst, by the late Robert Burpee, gives an account ofthe barotropic forecasting model that Sanders developedwith him, and that was in operational use for some twodecades for predicting the paths of tropical cyclones. Thenext (Gyakum) discusses cold-season precipitation eventsin the northeastern USA, and the insight that Sandersprovided for predicting them. Then an article ‘Must Sur-prise Snowstorms be a Surprise?’ (Tracton) considers thesource and nature of uncertainties in forecasts, in particu-lar East Coast snowstorms. With recent developments inensemble forecasting, the answer is essentially ‘no’. Thechange in thinking amongst operational forecasters, fromdeterministic to probabilistic forecasting, is noted. Part 3ends with a paper (Uccellini, Kocin, Sienkiewiczi, Kistlerand Baker) on Sanders’ many contributions to synopticmeteorology. The authors revisit the New York snow-storm of 26 December 1947, missed by the public forecastbut anticipated by Fred Sanders, who was then workingat La Guardia Airport. They simulated the storm with a

Copyright c© 2009 Royal Meteorological Society

Page 2: Synoptic–Dynamic meteorology and weather analysis and forecasting: a tribute to Fred Sanders, edited by Lance F. Bosart and Howard B. Bluestein. Meteorological Monograph Vol. 33

BOOK REVIEW 1915

modern NWP system. Lack of observations limited thepredictability of this event. The authors concluded thatSanders was ‘56 years ahead of his time!’

Part 4, on Climate and Climatology, opens with a 52-page article (Dole) on the linkage between weather andclimate. The emphasis is on the processes that bridgethe time-scales between synoptic events and seasonaland longer climate developments, and a broad range ofobserved variations and theoretical models are reviewed.The concluding chapter (Galarneau, Bosart and Aiyyer)looks at closed anticyclones, often associated with heat-waves and droughts.

There is a pictorial section with fifty photographsfeaturing many of Sanders’ students and collaborators.An Appendix, written by Sanders himself, outlines his

‘Career with Fronts: Real Ones and Bogus Ones’. Helooks at changing views on frontal theory over the courseof his career, and concludes that, even in present-dayoperational analysis, a distinction between features thatagree with the Norwegian conceptual model and thosethat do not, is essential.

The book is nicely produced, in large format on high-quality paper. It contains much of interest to anyoneinvolved in synoptic meteorology. It will be of specialinterest to those of us who knew Sanders or who admirehis work. There is some repetition, unavoidable in a bookof this nature. The book contains much material that couldbe of value in teaching. However, with its high cost andinhomogeneous content and style, it is not suitable as atext book.

PETER LYNCHProfessor of Meteorology,

University College Dublin.

Copyright c© 2009 Royal Meteorological Society Q. J. R. Meteorol. Soc. 135: 1914–1915 (2009)DOI: 10.1002/qj