Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1175/JAS-D-18-0142.1 |
Stability and Sea State as Limiting Conditions for TKE Dissipation and Dissipative Heating | |
Smith, Andrew W.1; Haus, Brian K.1; Zhang, Jun A.2,3 | |
2019-03-01 | |
发表期刊 | JOURNAL OF THE ATMOSPHERIC SCIENCES
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ISSN | 0022-4928 |
EISSN | 1520-0469 |
出版年 | 2019 |
卷号 | 76期号:3页码:689-706 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | This study analyzes high-resolution ship data collected in the Gulf of Mexico during the Lagrangian Submesoscale Experiment (LASER) from January to February 2016 to produce the first reported measurements of dissipative heating in the explicitly nonhurricane atmospheric surface layer. Although typically computed from theory as a function of wind speed cubed, the dissipative heating directly estimated via the turbulent kinetic energy (TKE) dissipation rate is also presented. The dissipative heating magnitude agreed with a previous study that estimated the dissipative heating in the hurricane boundary layer using in situ aircraft data. Our observations that the 10-m neutral drag coefficient parameterized using TKE dissipation rate approaches zero slope as wind increases suggests that TKE dissipation and dissipative heating are constrained to a physical limit. Both surface-layer stability and sea state were observed to be important conditions influencing dissipative heating, with the stability determined via TKE budget terms and the sea state determined via wave steepness and age using direct shipboard measurements. Momentum and enthalpy fluxes used in the TKE budget are determined using the eddy-correlation method. It is found that the TKE dissipation rate and the dissipative heating are largest in a nonneutral atmospheric surface layer with a sea surface comprising steep wind sea and slow swell waves at a given surface wind speed, whereas the ratio of dissipative heating to enthalpy fluxes is largest in near-neutral stability where the turbulent vertical velocities are near zero. |
英文关键词 | Turbulence Surface layer Air-sea interaction Energy budget/balance Ship observations Spectral analysis/models/distribution |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000459006400002 |
WOS关键词 | TURBULENT KINETIC-ENERGY ; ATMOSPHERIC SURFACE-LAYER ; BOUNDARY-LAYER ; WIND ; MOMENTUM ; VARIANCE ; BUDGET ; SWELL ; FLUX |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/29232 |
专题 | 地球科学 |
作者单位 | 1.Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, 4600 Rickenbacker Causeway, Miami, FL 33149 USA; 2.Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA; 3.NOAA, AOML, Hurricane Res Div, Miami, FL USA |
推荐引用方式 GB/T 7714 | Smith, Andrew W.,Haus, Brian K.,Zhang, Jun A.. Stability and Sea State as Limiting Conditions for TKE Dissipation and Dissipative Heating[J]. JOURNAL OF THE ATMOSPHERIC SCIENCES,2019,76(3):689-706. |
APA | Smith, Andrew W.,Haus, Brian K.,&Zhang, Jun A..(2019).Stability and Sea State as Limiting Conditions for TKE Dissipation and Dissipative Heating.JOURNAL OF THE ATMOSPHERIC SCIENCES,76(3),689-706. |
MLA | Smith, Andrew W.,et al."Stability and Sea State as Limiting Conditions for TKE Dissipation and Dissipative Heating".JOURNAL OF THE ATMOSPHERIC SCIENCES 76.3(2019):689-706. |
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