Linear Time-Invariant Models of a Large Cumulus Ensemble

被引:0
|
作者
Kuang, Zhiming [1 ,2 ]
机构
[1] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
[2] Harvard Univ, Sch Engn & Appl Sci, Cambridge, MA 02138 USA
关键词
Convective adjustment; Deep convection; Convective parameterization; Machine learning; BOUNDARY-LAYER CLOUDS; PDF-BASED MODEL; STRATIFORM INSTABILITY; PART I; CLIMATE; IDENTIFICATION; EQUILIBRIUM; TEMPERATURE; CONVECTION; WAVES;
D O I
10.1175/JAS-D-23-0194.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Methods in system identification are used to obtain linear time -invariant state-space models that describe how horizontal averages of temperature and humidity of a large cumulus ensemble evolve with time under small forcing. The cumulus ensemble studied here is simulated with cloud-system-resolving models in radiative- convective equilibrium. The identified models extend steady-state linear response functions used in past studies and provide accurate descriptions of the transfer function, the noise model, and the behavior of cumulus convection when coupled with two-dimensional gravity waves. A novel procedure is developed to convert the state-space models into an interpretable form, which is used to elucidate and quantify memory in cumulus convection. The linear problem studied here serves as a useful reference point for more general efforts to obtain data -driven and interpretable parameterizations of cumulus convection.
引用
收藏
页码:605 / 627
页数:23
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