Gerard Kilroy

Gerard Kilroy



Department of Physics, Meteorological Institute, University of Munich (LMU), Theresienstr. 37, 80333 Munich
Email: gerard.kilroy@lmu.de



Lectures


Publications

(2) KILROY G, Smith RK, and Wissmeier U. 2014:
    Tropical cyclone convection: the effects of ambient vertical and horizontal vorticity
   
Quart. J. Roy Meteor. Soc., 140, 1756-1770.

(3) KILROY G, and Smith RK, 2014:
    Tropical-cyclone convection: the effects of a vortex boundary layer wind profile on deep convection
   
Quart. J. Roy. Meteor. Soc. 141, 714-726.

(4) Smith RK, KILROY G, and Montgomery MT, 2015:
    Why do model tropical cyclones intensify more rapidly at low latitudes?
   
J. Atmos. Sci., 72, Issue 5 (May 2015) pp. 1783-1804.

(5) Smith RK, Montgomery MT, KILROY G, Tang D, and Müller S, 2015:
    Tropical low formation during the Australian monsoon: the events of January 2013.
   
Aust. Meteor. Ocean. Journl., 65, 318-341.

(6) KILROY G, Smith RK and Montgomery MT, 2016:
    Why do model tropical cyclones grow progressively in size and decay in intensity after reaching maturity?
   
J. Atmos. Sci., 73, 487-503.

(7) Črnivec N, Smith RK and KILROY G, 2016:
    Dependence of tropical cyclone intensification rate on sea surface temperature.
   
Quart. J. Roy. Meteor. Soc., 142, 1618-1627.

(8) KILROY G, Smith RK, Montgomery MT, Lynch B and Earl-Spurr C, 2016:
    A case study of a monsoon low that formed over the sea and intensified over land as seen in the ECMWF analyses
   
Quart. J. Roy. Meteor. Soc., 142, 2244-2255.

(9) KILROY G and Smith RK, 2016:
    A numerical study of deep convection in tropical cyclones
   
Quart. J. Roy. Meteor. Soc., 142, 3138-3151.

(10) KILROY G, Smith RK and Montgomery MT, 2017:
    A unified view of tropical cyclogenesis and intensification.
   
Quart. J. Roy. Meteor. Soc., 143, 450-462.

(11) KILROY G, Smith RK and Montgomery MT, 2017:
    Tropical low formation and intensification over land as seen in ECMWF analyses.
   
Quart. J. Roy. Meteor. Soc., 143, 772-784.

(12) KILROY G,Montgomery MT and Smith RK, 2017:
    The role of boundary-layer friction on tropical cyclogenesis and intensification.
   
Quart. J. Roy. Meteor. Soc. 143, 2524-2536.

(13) KILROY G and Smith RK MT, 2017:
    The effects of initial vortex size on tropical cyclogenesis and intensification
   
Quart. J. Roy. Meteor. Soc. 143, 2832–2845.

(14) KILROY G, Smith RK and Montgomery MT, 2018:
    The role of heating and cooling associated with ice processes on tropical cyclogenesis and intensification
   
Quart. J. Roy. Meteor. Soc. 144, 99-114.

(15) Smith RK, Montgomery MT and KILROY G, 2018:
    The generation of kinetic energy in tropical cyclones revisited
   
Quart. J. Roy. Meteor. Soc. 144, 2481-2490.

(16) Steenkamp SC, KILROY G, Smith RK, 2019:
    Tropical cyclogenesis at and near the Equator.
   
Quart. J. Roy. Meteor. Soc. (early view).

(17) Raymond D and KILROY G, 2019:
    Control of Convection in High-Resolution Simulations of Tropical Cyclogenesis.
   
J. Adv. Model. Earth Syst., (early view).

(18) KILROY G, Smith RK and Montgomery MT, 2019:
    An idealized numerical study of tropical cyclogenesis at the Equator
   
J. Adv. Model. Earth Syst., (submitted).


Academic CV


Scientific Activities, Conferences, Summer schools




Current Work