00000nam 2200000za 4500 9.868077 CaOODSP 20241203113645 m go d f cr ||||||||||| 190207s1978 bcc fo f000 0 eng d CaOODSP eng CaOODSP rda n-cn-bc En57-44/78-024E-PDF Haering, Peter, author. The effect of analyses on subsequent prognoses : a subjective evaluation / Pete Haering, meteorologist. Vancouver : Pacific Weather Centre, [1978]. 1 online resource (4 unnumbered pages). text txt rdacontent computer c rdamedia online resource cr rdacarrier Pacific region technical notes ; no. 78-024 Caption title. Continued by: The effect of analyses on subsequent prognoses cont. : 1. upper level flow patterns 2. the cut-off low [En57-44/78-027E-PDF] ; The effect of analyses on subsequent prognoses cont. : 1. erroneous vorticity pattern 2. lack of data [En57-44/78-029E-PDF] ; The effect of analyses on subsequent prognoses cont. : 1. good analyses lead to good prognoses 2. erroneous vorticity patterns at edge of wind field [En57-44/78-030E-PDF] ; The effect of analyses on subsequent prognoses cont. : erroneous intensities of correctly located vorticity patterns [En57-44/78-031E-PDF]. Digitized edition from print [produced by Environment and Climate Change Canada]. "GOES satellite imagery can be used to assess initial upper air analyses (500 mb. and 250 mb.) over the eastern Pacific. .. the imagery can be used to gain much useful informaation as to the intensity and extent of the major trofs by examining the nature of the convective clouds. Such an examination will then indirectly lead towards and assessment of thickness patterns over the sparse ocean data areas." gccst Weather forecasts gccst Satellite imagery Canada. Environment Canada. Canada. Atmospheric Environment Service. Pacific Region. Canada. Atmospheric Environment Service. Pacific Weather Center. The effect of analyses on subsequent prognoses cont. : 1. upper level flow patterns 2. the cut-off low. The effect of analyses on subsequent prognoses cont. : 1. erroneous vorticity pattern 2. lack of data. The effect of analyses on subsequent prognoses cont. : 1. good analyses lead to good prognoses 2. erroneous vorticity patterns at edge of wind field. The effect of analyses on subsequent prognoses cont. : erroneous intensities of correctly located vorticity patterns. Pacific region technical notes (Canada. Atmospheric Environment Service. Pacific Region) no. 78-024 (CaOODSP)9.865532 PDF 2.02 MB https://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-78-024-eng.pdf