div class=ts-pagebuttonPage 1button div class=ts-image amp-img class=ts-thumb alt=Page 1: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails1jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 2button div class=ts-image amp-img class=ts-thumb alt=Page 2: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails2jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 3button div class=ts-image amp-img class=ts-thumb alt=Page 3: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails3jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 4button div class=ts-image amp-img class=ts-thumb alt=Page 4: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails4jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 5button div class=ts-image amp-img class=ts-thumb alt=Page 5: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails5jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 6button div class=ts-image amp-img class=ts-thumb alt=Page 6: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails6jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 7button div class=ts-image amp-img class=ts-thumb alt=Page 7: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails7jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 8button div class=ts-image amp-img class=ts-thumb alt=Page 8: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails8jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 9button div class=ts-image amp-img class=ts-thumb alt=Page 9: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails9jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 10button div class=ts-image amp-img class=ts-thumb alt=Page 10: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails10jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 11button div class=ts-image amp-img class=ts-thumb alt=Page 11: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails11jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 12button div class=ts-image amp-img class=ts-thumb alt=Page 12: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails12jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 13button div class=ts-image amp-img class=ts-thumb alt=Page 13: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails13jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 14button div class=ts-image amp-img class=ts-thumb alt=Page 14: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails14jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 15button div class=ts-image amp-img class=ts-thumb alt=Page 15: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails15jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 16button div class=ts-image amp-img class=ts-thumb alt=Page 16: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails16jpg width=142 height=106 layout=responsive amp-img divdivdiv class=ts-pagebuttonPage 17button div class=ts-image amp-img class=ts-thumb alt=Page 17: coreacuk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations The dominant synoptic feature was an intense src=https:reader033vdocumentinreader033viewer20220420075e707305bb46ab33bd14173ehtml5thumbnails17jpg width=142 height=106 layout=responsive amp-img divdiv