In the previous survey (Smithson, 1989), comments were made about the occasional nature of the appearance of books on the theme of microand mesoclimatology. Since then, two books have been published which, whilst being explicitly concerned with meteorology, do contain much information of use to climatologists. The larger book, by Stull (1988), is intended primarily as a textbook on boundary-layer meteorology, but it also serves as a reference book on present knowledge of atmospheric turbulence and boundary-layer processes, and as a literature review for these areas. Whilst much of this book is inevitably concerned with the physical processes operating in the boundary layer, it nevertheless provides very useful information about the causative factors behind many microclimatological features. In addition, a review is provided of boundarylayer sensing devices such as radar, sodar, lidar and various instrument platforms together with comments about their relative advantages and disadvantages. If one has the financial support to purchase, maintain and operate such equipment then this book will give guidance on which system would be most appropriate for a particular problem. The other book (Hsu, 1988) is specifically concerned with coastal meteorology, though the first four chapters are devoted to atmospheric physics which would be relevant for any scale. Physical processes in the boundary layer are discussed in some detail before the core is reached on air-sea-land . interaction. The final chapter on engineering meteorology reflects the origin of the book which was based on a course for students in science and engineering in the Department of Marine Sciences at Louisiana State University. As a result, Atkinson's much broader review of mesoscale circulation systems (Atkinson, 1981) still provides the best climatological reference in this area.Other publications will be discussed within the same subject framework as in the previous survey (Smithson, 1989).
I Instrumentation and techniquesInstrumentation of the meso-and microscales can range from satellite sensing down to eddy correlation methods used almost in contact with the ground surface.