ATMS 410 - Final Project

RESULTS

Description

Project theme music (Option#1)

Project theme music (Option#2)

Table template

GRVT         =            GAVA                                +               LTHAD                   + LAD  +  LDIA

Case study maps

    Base map

    GARP functions, contour intervals, and scale factors used in creating these maps

    1000 hPa maps at initial time

        Geo. Ht and Geostrophic Absolute Vorticity [purple contours; 4x10-5 s-1, s.f.=5]

        Geo. Ht and 10 meter Wind Speed   [green contours; 3 m s-1, s.f.=0]

    500 hPa maps at all times (P1 - P6, every six hours)

        Geostrophic Absolute Vorticity [4x10-5 s-1, s.f.=5]

            P1 P2 P3 P4 P5 P6

        1000-500 hPa Thickness [5120 & 5460 m contours only]

            P1 P2 P3 P4 P5 P6

        GAVA [shading, s.f.=9]

            P1 P2 P3 P4 P5 P6

        nearly LTHAD [shading, s.f.=13] {need to multiply values on these maps by " -g/f " to get LTHAD}

            P1 P2 P3 P4 P5 P6

        nearly LAD [shading, s.f.=13] {need to multiply values on these maps by " -g s /f " to get LAD}

            P1 P2 P3 P4 P5 P6

    700 hPa maps at all times (P1 - P6, every six hours)

        fields related to LDIA (using 700 hPa omega) [2 mb s-1, s.f.=3]

            unshaded omega (black) represents NEGATIVE omega

            RH is 1000-700 layer-averaged value [10%, s.f.=0]

            ASSUME that LDIA has the same sign ["+" or "-"] as diabatic heating

            P1 P2 P3 P4 P5 P6

Email inquiries

         noon, Monday, November 23, 2015; deadline for inquiries

Email#01

Email#02

Email#03

Email#04

THAD = thickness (temperature) advection

or

this guy