Shear-Parallel Mesoscale Convective Systems in a Moist Low- Inhibition Mei-Yu Front Environment. Liu and Moncrieff (2017 JAS)
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1 Shear-Parallel Mesoscale Convective Systems in a Moist Low- Inhibition Mei-Yu Front Environment Liu and Moncrieff (2017 JAS)
2 Introduction Balance of lower-tropospheric wind shear and strength of evaporation-generated cold pool is highly important in governing TS squall line organization (Rotunno et al. 1988; RKW theory) For other types of convective systems (eg. TL-AS MCS), the mechanism regulating their organization (eg. back-building) is highly dependent on near-surface cold outflow (Parker 2007a) Role of cold pool much more uncertain in Mei-yu front environment! Crucial characteristic of mei-yu front environment is the nearly-saturated low troposphere -> Limited evaporative cooling and weakened density current Past results on MCSs in near-saturated environments i. Lack of cold pool forcing increases the importance of other processes (eg. mesoscale forcing. gravity wave) [Crook and Moncrieff 1988] ii. Studies for quasi-stationary heavily raining MCS suggests that convectively-generated gravity wave forcing is influential for flow organization [Schumacher and Johnson 2008; Schumacher 2009, 2015] iii. Fovell et al. (2006) has established the relationship between gravity wave forcing and the observed "convective initialization prior to squall line gust front" phenomenon
3 Experiment Design WRF model [2401x1801x101 grid points, (0.5km horizontal, 0.2km vertical) Sounding used previously by Yamasaki (2009) used to simulate a 2004 mei-yu rainband, under strong westerly shear Mei-yu environment is approximated by the following perturbation equations: Initialized sounding These equations define a 200-km-wide moisture front, corresponding to a Tv gradient of ~0.3K/100km 1 sensitivity test (No rainwater evaporative cooling)
4 Does weak cold pool play a role? System evolution similar to CTRL (initial downstream propagation due to ambient wind advection -> quasistationary -> slow upstream propagation) MCS is narrower than CTRL and extends further upstream Hypothesis Turning off rainwater evaporation -> Less diabatic cooling to neutralize latent heat release-> Stronger MCS Much heavier precipitation and precipitation seems to be "locked" along moisture front Shear-parallel, quasi-stationary, elongated rainband is produced is both simulations
5 Surface precipitation Strong convective precip centered on moisture front, weak stratiform precip downstream Quasi-stationary MCS moves upstream slowly due to repeated convective initiation The overall structure similar to backbuilding/parallel-stratiform MCS (Parker 2007a,b; Wang et al. 2014) The MCS is characterized by "upstream building" as cells regenerate to the east of MCS system
6 Mesoscale kinematic and thermodynamic characteristics (a) Condensate (shading, g/kg) and u-wind perturbation (contours) (b) Vertical Velocity (shading, m/s) and RH (contours) (c) Potential temperature perturbation (shading, oc) (d) Pressure perturbations (shading, Pa) Houze et al. 1989
7
8 Gravity-waves-generated lifting ront n=1+2 heating Nicholls et al. (1991) Gust f n=1 heating Fovell et al. (2006)
9 Does weak cold pool play a role? (e) Condensate (shading, g/kg) and u-wind perturbation (contours) (f) Vertical Velocity (shading, m/s) and RH (contours) (g) Potential temperature perturbation (shading, oc) (h) Pressure perturbations (shading, Pa) Seems not!
10 Gravity wave activity I. Upstream-propagating deep mode 04hr 2nd Gravest mode 5.5hr Gravest mode Vertical Velocity [Contours - Updraft (solid), downdraft (dashed)] Potential Temperature Perturbation (Shading) Relative Humidity >98% (Green Contours at 5.5hr) Cloud Boundary (Black Contours at 5.5hr)
11 Gravity wave activity I. Upstream-propagating deep mode LCL~ m LFC~ m Trajectories of 200 parcels released upstream of MCS (a) Altitude time in W-E direction (b) Altitude changes with time
12 Gravity wave activity II. Downstream-moving slow mode 06hr
13 Gravity wave activity II. Downstream-moving slow mode Vertical Velocity (Contours, cm/s) Potential temperature perturbation (shading) X-axis wind component (contours, m/s) Cloud Boundaries (Green contours)
14 Gravity wave activity II. Downstream-moving slow mode 8.5hr 10hr 9.5hr 1km vertical velocity (cm/s)
15 Gravity wave activity II. Downstream-moving slow mode Propagating Mode Temperature Advection Diabatic heating
16 Gravity wave activity II. Downstream-moving slow mode Growing Mode If there is no phase difference between Q, w' (beta=0) Either: (1) ci=0 (disturbance cannot amplify) (2) U-cr=0 (Existence of critical level)
17 Gravity wave activity II. Downstream-moving slow mode Upstream scorer parameter across moisture front (10^-6 m^-2)
18 Summarizing gravity wave's role H High-frequency GW Destabilizes environment (cooling tendency in moist low troposphere, creating shallow cloud deck upstream) L Low-frequency GW Triggering boundary layer cumulus cloud within the preconditioned saturated layer Disparities between simulated system and Fovell et al. (2006) New CI triggered ahead of gust front can be harmful to F06's system by undercutting unstable air inflow; GW cell triggering is vital in this study GWs in F06 originated from parent storm, move upstream, trigger new convection; Highfrequency GWs in this study is excited upstream by boundary layer cumulus and moves downstream by ambient wind Wave-ducting mechanism in F06 is uppertropospheric outflow from MCS; Background flow curvature in this study
19 Some remaining issues & MCS 3D structure Line-normal wind (contour+vector) averaged between h Line-parallel (u-wind) momentum transport vertical profile along moisture front
20 Some remaining issues & MCS 3D structure Throughflow Up-down flow Jump updraft Jump downdraft Rear-to-front downdraft completely absent in simulated MCS MCS propagates in wavelike manner Most boundary layer parcels are transported to 12-14km by jump updraft, a portion descends in updown flow Most parcels above 6km traverse system in throughflow branch with small lifting 3D spatial & airflow structure, wavelike propagation similar to Moncrieff and Lane (2015) Upstream-building, shear-parallel evolution and strong transverse circulation resemble Dudhia and Moncrieff (1987), Khouider and Moncrieff (2015)
21 THE END Thank you for listening
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