journal articleLitStream CollectionEditorialWalker, Gilbert T.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326801pmid: N/A
journal articleLitStream CollectionReport on the phenological observations in the British isles from December 1934 to November 1935Margary, Ivan D.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326802pmid: N/A
journal articleLitStream CollectionThe application of wet‐bulb potential temperature to air mass analysis. II the ascent of air at warm frontsHewson, E. W.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326803pmid: N/A
journal articleLitStream CollectionErratum1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326804pmid: N/A
journal articleLitStream CollectionThe presentation of visibility observations: Visibility characteristic curves and a visibility indexPoulter, R. M.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326805pmid: N/A
journal articleLitStream CollectionOn the emission of the sky during twilight and during the eclipse totality of 1936, June 19: Preliminary note by D. J. EropkinChapman, S.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326806pmid: N/A
journal articleLitStream CollectionThe formation of coloured rainBoyden, C. J.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326807pmid: N/A
journal articleLitStream CollectionBlue colour of the sun and surrounding sky in a dust stormDurward, J.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326808pmid: N/A
journal articleLitStream CollectionRainfall over the rivington catchment areaLloyd, David1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326809pmid: N/A
journal articleLitStream CollectionWhat can submarine canyons tell us about the character of the great ice age?Whipple, F. J. W.1937 The Quarterly Journal of the Royal Meteorological Societydoi: 10.1002/qj.49706326810pmid: N/A