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Howard B. Bluestein

520 MONTHLY WEATHER REVIEW VOLUME 113An Observational Study of a Mesoscale Area of Convection under Weak Synoptic-Scale Forcing HOWARD B. BLUESTEINUniversity of Oklahoma, School of Meteorology, Norman, OK 73019(Manuscript received 6 April 1984, in final form 30 November 1984)ABSTRACT This is a case study of a mesoscale area of convection which began at night over western Kansas on 2

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Montreal p h c ........ 13 Nluhville' enn .......... 15 Fort Ellidtt, Tex ........ 19 Portland, Mo ............. 20 2 Fort Bully, 8. Dnk ........ aa 4615................... Choyenne, Wyo 3 4 8Lacrosse, Wia .......... 60Medicine Hat, N. W. T..l z: I64............................... I 1 5 7- d .-E 5nw. nw.ne.nw!nw.nw. nw. n. nw. ne.-aw.....aw. aw.W.W.W.W.W.W.aw.W.SW.8.nw.nw..... -............................... I0 NORTH ATLANTIC STORMS FOR JANUARY, 1890 (pressure iu inches and millimetres; wind-force by

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S. F. Milton and C. A. Wilson

SEPTEMBER 1996 MILTON AND WILSON 2023The Impact of Parameterized Subgrid-Scale Orographic Forcing on Systematic Errors in a Global NW? Model S. F. MILTON AND C. A. WILSONU.K. Meteorological Office, Bracknell, United Kingdom(Manuscript received I 1 October 1995, in final form 6 February 1996)ABSTRACT The global momentum budget for December 1993, diagnosed from a series of

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Pacific coast on the 26th. It passed eastward as far as Manitoba, where it was central atthe close of the month, but the pressure had increased at the centre during the easterly movement.FEBEUARY, 1889.N,ORTH ATLANTIC STORMS FOR FEBRUARY, 1889 (pressure in iuches and millimetres ; wind-force by Beaufort scale).The paths of the depressions that appeared over the nortt Atlantic Ocean during February, 1889, are shown on chart iThese paths have been determined from international simul taneous observations

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V. A. Mousseau, D. A. Knoll, and J. M. Reisner

1. Introduction An implicit nonlinearly consistent (INC) solution method is presented for the solution of the shallow-water equations including the Coriolis force in two-dimensions. We demonstrate that a second-order-in-time INC method can provide accurate solutions to problems even when the advective Courant–Friedrichs–Lewy (CFL) number is greater than one. To explain this result we performed an approximate modified equation analysis (AMEA) to quantify the differences between an INC solution

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J. Egger

AemL1976 J. EGGER 351The Linear Response of a Hemispheric Two-Level Primitive Equation Model to Forcing by Topography J.Institut f~r Theoretische Meteorologie, der Universit~t Miinchen, 8 M~nchcn, FRG (Manuscript received 14 August 1975, in revised form 23 October 1975) ABSTRACT A hemispheric solution is obtained for the

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., lath, wind shifted to north- westl increasing in force to a gale.(f?rty-eight miles) beiween 8 and 4 a. m.,continuing high all day and diminishing in force during the afternoon. Thechange in wind shortly crfter midnight corresponded with lowest barometer, 28.86 actual. The rise in the barometer after 1 a. m. was as rapid as hadbeen its fall during the preceding day. The chan e in barometric pressureis re resented by nn invertcd cone, with depth of1.6 inches. Rain ended shorlfy after midnight

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N. 26O, W. 76O, by the 21st. On this~ ~~~~date south to west gales of hurricane force prevailed over the eastern portion of the Bahama lalands; in the vicinity of the thirtieth parallel fresh easterly gales were reported, while off the Florida coast strong northerly gales prevailed. During the 22d and 23d the storm recurved slowly northward, with a marked decrease in energy; .by the 24th i t had advanced to N. 32O, W. 76O, and during $6 northeast passage along tliecourse of the Gulf Stream dur1n

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. fomia, Nevctda, Utah, and western Colorado, where i t wascentral on the 15th. Aftor the morning of the 15th tlieeasterljmovement became accelerated and by morning of the 16th thestofm was central in soiitliern Minncsota. I t increased iu force as It passed over Lake Superior, the barometer reaching the minimum ou the afternooil of the lfith, at Prince Arthurr Landing, when the caritre wa8 near that station. The area ol Precipitation included the whole countrY.east of the Rockj Mountains, the rains

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east Gulf coast, ;ii::::: on the morning of the 24th. After passing inland the winds I VIII .... diminished in force and i t mored off the North C;wolina coast as a disturbance of slight energy, although the report,s from the Atlantic and from Sydney, C. B. I., of the 26th indicate,these low areas:. -.No.... . -. .iI Lowest prossure. L---.-M.- .- b d ! Stntion. J*I. d-d-.-.- 2 ,E : ...--. . .- - ... . -.Inches.29.3'3NORTH ATLAKTIC STORMS FOR MARCH, 1889 (pressure in inches and millimetres; mind-force

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