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ارزیابی عملکرد یک طرح‌واره لایه مرزی سیاره‌ای با استفاده از آزمایش GABLS1 در نسخه تک‌ستونی مدل جهانی توسعه‌یافته برمبنای تاوایی پتانسیلی | ||
| فیزیک زمین و فضا | ||
| مقاله 6، دوره 47، شماره 2، مرداد 1400، صفحه 285-300 اصل مقاله (732.01 K) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/jesphys.2021.313768.1007261 | ||
| نویسندگان | ||
| میلاد بهروش1؛ علیرضا محب‌الحجه2؛ محمد میرزائی* 3؛ دانیال یازجی4 | ||
| 1دانشجوی دکتری، گروه فیزیک فضا، مؤسسه ژئوفیزیک، دانشگاه تهران، تهران، ایران | ||
| 2استاد، گروه فیزیک فضا، مؤسسه ژئوفیزیک، دانشگاه تهران، تهران، ایران | ||
| 3استادیار، گروه فیزیک فضا، مؤسسه ژئوفیزیک، دانشگاه تهران، تهران، ایران | ||
| 4پژوهشگر، گروه تحقیقات، مؤسسه هواشناسی و آب‌شناسی سوئد، نورشوپینگ، سوئد | ||
| چکیده | ||
| شبیه‌سازی درست ساختار لایه مرزی جو به‌ویژه در شرایط پایدار از موضوعات چالش‌انگیز در مدلهای عملیاتی جوی است. آزمایش‌های مقایسه متقابل مدل‌ها همچنان اختلاف‌های شایان‌‌‌توجهی را در پیش‌بینی متغیرهای لایه مرزی جو در مدلهای عملیاتی و تحقیقاتی نشان می‌دهند. در این مطالعه، یک طرح‌واره لایه مرزی مرتبه ۵/۱ برای ارزیابی عملکرد پیوند آن با هسته دینامیکی مدل جهانی دانشگاه تهران (UTGAM) با کاربست نسخه تک‌ستونی مدل یادشده و استفاده از آزمایش‌های استاندارد مقایسه متقابل GABLS1 بررسی شده است. همچنین، عملکرد مختصات قائم سیگما-تتا و سیگما-پی در دو حالت با تفکیک‌پذیری قائم مختلف ۱۴ و ۳۳ تراز تا زیر ارتفاع ۳ کیلومتر ارزیابی شد. در مجموع اختلافی جزئی بین مختصات سیگما-تتا و سیگما-پی در حالت‌های تفکیک پایین با هم و همچنین حالت‌های تفکیک بالا با هم مشاهده شد که این اختلاف در تفکیک‌پذیری پایین بیشتر نمایان است. در هر دو مجموعه از آزمایش‌‌ها، بهبود نتایج شبیه‌سازی‌ها با افزایش تفکیک‌پذیری هویدا است. علاوه‌بر اینها به‌نظر می‌رسد که نزدیک‌تر کردن موقعیت قرارگیری پایین‌ترین تراز صحیح از سطح در حالت با تفکیک‌پذیری بالا بر بهبود نتایج در این حالت مؤثر بوده است. مقایسه نیم‌رُخ قائم باد با سایر مدلهای عملیاتی شرکت‌کننده در آزمایش GABLS1 عملکرد بهتر طرح‌واره لایه‌مرزی استفاده‌شده در این پژوهش را نشان می‌دهد اما برای نیم‌رُخ قائم دمای پتانسیلی در ارتفاعات پایین، اُریبی محسوس منفی شبیه‌سازی شده است. برطبق نتایج، طرح‌واره لایه مرزی استفاده‌شده همچون سایر مدلهای عملیاتی پیش‌بینی وضع هوا، برای شرایط پایدار پخش تکانه و گرما را بیش‌برآورد می‌کند. | ||
| کلیدواژه‌ها | ||
| شبیه‌سازی؛ GABLS1؛ لایه مرزی پایدار؛ مختصات قائم؛ ضرایب پخش؛ UTGAM | ||
| عنوان مقاله [English] | ||
| Evaluating the performance of a planetary boundary layer scheme using GABLS1 experiment in a single-column version of the global model developed based on potential vorticity | ||
| نویسندگان [English] | ||
| Milad Behravesh1؛ Ali Reza Mohebalhojeh2؛ Mohammad Mirzaei3؛ Danial Yazgi4 | ||
| 1Ph.D. Student, Department of Space Physics, Institute of Geophysics, University of Tehran, Tehran, Iran | ||
| 2Professor, Department of Space Physics, Institute of Geophysics, University of Tehran, Tehran, Iran | ||
| 3Assistant Professor, Department of Space Physics, Institute of Geophysics, University of Tehran, Tehran, Iran | ||
| 4Researcher, Research department, Swedish Meteorological and Hydrological Institute, Norrköping, Sweden | ||
| چکیده [English] | ||
| Representing the boundary layer processes is crucial in simulating atmospheric phenomena in operational hydrostatic weather forecast models. Moreover, evaluating the performance of different physical processes in a variety of numerical models is an essential subject of its own. This paper presents an objective assessment of a planetary boundary layer scheme based on turbulent kinetic energy in a single-column version of the innovative atmospheric general circulation model developed based on potential vorticity at the University of Tehran, which is called UTGAM. Single-column models are a complementary tool to the atmospheric general circulation models that provide a simple framework to investigate the fidelity of the simulated physical processes. The reliable parameterization of the boundary layer processes has got significant impacts on weather forecasts. Most of the hydrostatic models have got deficiencies in the representation of these unresolved processes, especially in stably stratified conditions, and it seems that this problem is continuing in the forthcoming future. Here we have utilized the first GABLS intercomparison experiment set up as a simple tool to evaluate the performance of the diffusion scheme in the UTGAM. Two different sigma-theta and sigma-pressure single-column grid staggering combined with, respectively, 33 and 14 vertical levels below 3 km height have been used for the low- and high-resolution simulations. The GABLS1 LES results have been used as a benchmark for comparison. The boundary layer scheme that has been explored here is the same as the one in the ECHAM model, but some simplifications have been made. For instance, in this simulation, the effects of tracers have been ignored to circumvent the complexity of the problem. Results depict subtle nuances between the sigma-theta and sigma-pressure coordinates in intercomparison between the low and high vertical resolutions separately, which are more apparent in the lower vertical resolution. Nevertheless, it seems that the diffusion processes have been simulated rather more accurately in the high-resolution sigma-pressure vertical coordinate. The boundary layer scheme analogous with most of the operational models in the GABLS1 intercomparison experiment overestimate the momentum and the heat diffusion coefficients. The wind profile with height, depicts maxima that are higher than the corresponding LES profile. It is inferred that the scheme mixes momentum over a deeper layer than the LES, but the simulated wind profile is better in comparison with the other operational models in GABLS1. Considering the vertical profiles of potential temperature revealed that the amount of heat mixing is not suitable in this experiment, and it causes a negative bias in the lower part of the simulated boundary layer. The simulated amounts of surface friction velocity have proved significant differences with the LES results in all separate experiments. However, the latter large amounts seem unlikely to have a detrimental effect on forecast scores in the operational model. Moreover, the sensitivity of the scheme to the lowest full level has been partially explored. Decreasing the lowest full-level height concurrent with increasing the vertical resolution leads to a modest influence on the simulation of the boundary layer processes. All the results confirm notable improvements by increasing the vertical resolution in both sigma-theta and sigma-pressure coordinates. | ||
| کلیدواژه‌ها [English] | ||
| Simulation, GABLS1, stable boundary layer, vertical coordinate, diffusion coefficients, UTGAM | ||
| مراجع | ||
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