Kinetic Energy Budget for the Madden-Julian Oscillation in a Multiscale Framework

被引:33
作者
Zhou, Lei [2 ]
Sobel, Adam H. [1 ,3 ]
Murtugudde, Raghu [4 ]
机构
[1] Columbia Univ, Lamont Doherty Earth Observ, Dept Appl Phys & Appl Math, New York, NY USA
[2] SOA, SIO, State Key Lab Satellite Ocean Environm Dynam, Hangzhou, Zhejiang, Peoples R China
[3] Columbia Univ, Lamont Doherty Earth Observ, Dept Earth & Environm Sci, New York, NY USA
[4] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA
关键词
SYNOPTIC-SCALE DISTURBANCES; TROPICAL INTRASEASONAL OSCILLATIONS; TEMPERATURE-GRADIENT APPROXIMATION; CONVECTIVE MOMENTUM TRANSPORT; TOGA COARE IOP; PART I; MODEL; PACIFIC; WIND; CIRCULATION;
D O I
10.1175/JCLI-D-11-00339.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A kinetic energy budget for the Madden-Julian oscillation (MJO) is established in a three-scale framework. The three scales are the zonal mean, the MJO scale with wavenumbers 1-4, and the small scale with wavenumbers larger than 4. In the composite budget, the dominant balance at the MJO scale is between conversion from potential energy and work done by the pressure gradient force (PGF). This balance is consistent with the view that the MJO wind perturbations can be viewed as a quasi-linear response to a slowly varying heat source. A large residual in the upper troposphere suggests that much kinetic energy dissipates there by cumulus friction. Kinetic energy exchange between different scales is not a large component of the composite budget. There is a transfer of kinetic energy from the MJO scale to the small scale; that is, this multiscale interaction appears to damp rather than strengthen the MJO. There is some variation in the relative importance of different terms from one event to the next. In particular, conversion from mean kinetic energy can be important in some events. In a few other events, the influence from the extratropics is pronounced.
引用
收藏
页码:5386 / 5403
页数:18
相关论文
共 90 条
[1]   A new multiscale model for the Madden-Julian oscillation [J].
Biello, JA ;
Majda, AJ .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2005, 62 (06) :1694-1721
[2]   Climate and tropical cyclone activity: A new model downscaling approach [J].
Emanuel, Kerry .
JOURNAL OF CLIMATE, 2006, 19 (19) :4797-4802
[3]  
BLADE I, 1993, J ATMOS SCI, V50, P2922, DOI 10.1175/1520-0469(1993)050<2922:TIOIAS>2.0.CO
[4]  
2
[5]  
Bretherton CS, 2003, J ATMOS SCI, V60, P451, DOI 10.1175/1520-0469(2003)060<0451:TGMATW>2.0.CO
[6]  
2
[7]  
EMANUEL KA, 1987, J ATMOS SCI, V44, P2324, DOI 10.1175/1520-0469(1987)044<2324:AASIMO>2.0.CO
[8]  
2
[9]  
Ferreira RN, 1997, J ATMOS SCI, V54, P261, DOI 10.1175/1520-0469(1997)054<0261:BAOIB>2.0.CO
[10]  
2