the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part I: Understanding expressiveness of schemes for different regions from the mechanism perspective
Wenxing Jia
Xiaoye Zhang
Hong Wang
Yaqiang Wang
Deying Wang
Junting Zhong
Wenjie Zhang
Lei Zhang
Lifeng Guo
Yadong Lei
Jizhi Wang
Yuanqin Yang
Yi Lin
Abstract. The optimal choice of the planetary boundary layer (PBL) parameterization scheme is of particular interest and urgency to a wide range of scholars, especially for many works involving models. At present, there have been many works to evaluate the PBL schemes. However, little research has been conducted into a more comprehensive and systematic assessment of the performance capability of schemes in key regions of China, especially when it comes to the differences in the mechanisms of the schemes themselves, primarily because there’s scarcely sufficient observational data, computer resources, and storage support to complete the work. In addition, there are many factors that influence the selection of schemes, such as underlying surface, initial and boundary conditions, near-surface layer scheme, horizontal/vertical resolution, etc. In this Part (i.e., Part I), four typical schemes (i.e., YSU, ACM2, BL and MYJ) are selected to systematically analyze and evaluate near-surface meteorological parameters, PBL vertical structure, PBL height (PBLH), and turbulent diffusion in five key regions (i.e., North China Plain, NCP; Yangtze River Delta, YRD; Sichuan Basin, SB; Pearl River Delta, PRD and Northwest Semi-arid, NS) of China in different seasons (i.e., January, April, July and October). The differences in the simulated 2-m temperatures between the nonlocal closure schemes are mainly affected by the downward shortwave radiation, but to compare the nonlocal closure schemes with the local closure schemes, the effect of sensible heat flux needs to be further considered. In terms of temporal variation, the simulated results for July are better than the other three months, and the simulated results for nighttime are better than daytime. In terms of regional distribution, the temperature at stations with higher elevation is easily underestimated, while overestimated with lower elevation. The variation of relative humidity corresponds to temperature. The 10-m wind speed is under the influence of factors like the momentum transfer coefficient and the integrated similarity functions at night. The wind speeds are more significantly overestimated in the plains and basin, while less overestimated or even underestimated in the mountains, as a result of the effect on topographic smoothing in the model. Moreover, the overestimation of small wind speeds at night is attributable to the inapplicability of the Monin-Obukhov similarity theory (MOST) at night. The model captures the vertical structure of temperature well, while the wind speed is outstandingly overestimated below 1000 m, largely because of the turbulent diffusion coefficient (TDC). The difference between the MOST and the mixing length theory, PBLH and Prandtl number is cited as the reason for the difference between the TDC of the YSU and ACM2 schemes. The TDCs of the BL and MYJ schemes are affected by the mixing length scale, which of BL is calculated on the basis of the effect of buoyancy, while MYJ calculates it with the consideration of the effect of the total turbulent kinetic energy. The PBLH of the BL scheme is better than the other schemes because of the better simulation results of temperature. The difference in the PBLH by the YSU and ACM2 scheme mainly comes from the Richardson number and the jagged PBLH of the MYJ scheme is due to the coarse vertical resolution and the threshold value.
In general, to select the optimal scheme, it is necessary to offer different options for different regions with different focuses (heat or momentum). (1) Temperature field. The BL scheme is recommended for January in the NCP region, especially for Beijing, and the MYJ scheme is better for the other three months. The ACM2 scheme would be a good match for the YRD region, where the simulation differences between the four schemes are small. The topography of the SB region is more complex, but for most of the areas in the basin, the MYJ scheme is proposed, but if more stations outside the basin are involved, the BL scheme is recommended. The MYJ scheme is applied to the PRD region in January and April, and the BL scheme in July and October. The MYJ scheme is counselled for the NS region. (2) Wind field. The YSU scheme is recommended if the main concern is the near-surface layer, and the BL scheme is suggested if focusing on the variation in the vertical direction. The Part II will analyse and evaluate the factors that may influence the choice of the schemes and the results of model. The final evaluation of the parameterization scheme and uncertainties will lay the foundation for the improvement of the modules and forecasting of the GRAPES_CUACE regional model developed independently in China.
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Wenxing Jia et al.
Status: closed
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RC1: 'Comment on gmd-2023-30', Anonymous Referee #1, 28 May 2023
In the manuscript “Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part Ⅰ: Understanding expressiveness of schemes for different regions from the mechanism perspective” by Jia et al., the authors select four typical boundary layer parameterization schemes to systematically analyze and evaluate near-surface meteorological parameters, PBL vertical structure, PBLH, and turbulent diffusion in five key regions of China in different seasons. The work can be useful for other researchers to use as a reference when doing simulation studies. I have the following concerns that need to be addressed.
Specific comments:
(1) Abstract section: The abstract is too long and needs some reduction.
(2) Line 204-207: L-band radiosonde observations by the China Meteorological Administration are generally conducted twice a day (08:00 and 20:00 BJT), except for three times a day at individual stations in summer. More details information about the radiosonde observation data are required.
(3) The convective/unstable boundary layer is an important part of the study of planetary boundary layer. If there is no observation comparison of the daytime PBLH (14:00 BJT), does the author think that the evaluation of PBLH in different seasons in section 3.3 is insufficient.
(4) Lines 449-451: Please add the equation for calculating sensible heat flux (HFX) here, so that readers can directly understand the relationship between HFX and Ts-T2, and HFX and Ch.
(5) Lines 580-581: Add references to previous studies about wind speed, and explain how these results have been accepted by the public.
(6) Line 591 and 626: The YSU, ACM2 and BL schemes correspond to the revised MM5 near surface scheme and MYJ scheme correspond to another near surface scheme, right? If so, add the near surface scheme corresponding to MYJ scheme in Table 1.
(7) Lines 817-818: Regarding the criterion of the PBLH about the virtual potential temperature method, it seems the PBLH at dawn and dusk of the studied stations is at the transitional stage of the PBL (08:00 and 20:00 BJT). How can the authors prove that the determined PBLH is accurate and can be used to verify the simulation results of the BL scheme?
(8) Line 819 and 822: Please check that the equation number is correct.
(9) Lines 859-860: For the evaluation of MYJ scheme PBLH, the author uses virtual potential temperature method instead of TKE method. There may be some uncertainties due to different calculation criteria between observation and simulation.
(10) As the authors mentioned in the manuscript, there is currently insufficient observational data to calculate PBLH using TKE. What observations should be used to calculate PBLH using TKE? What is the calculation?
(11) Lines 870-871: This is a new attempt to analyze the turbulent diffusion coefficient. The current simulation results have not yet been verified by observations. While it would be strengthen the paper a lot if observational data can be included and analyzed.
(12) Line 871: “section 3.3.2” should be “section 3.2.2”.
(13) Figure 14 and 15: “Zhanjiakou” should be changed to “Zhangjiakou”.
(14) Figure 15: The caption is wrong, not 10-m wind speed and direction.
(15) Figure 16: What do "Ri", “PTv”, "PBLHOBS" and “two methods” stand for? It would be better to state this clearly in the caption.
(16) Figure 19: The resolution of the image is too low to distinguish the information shown in the image. And “SCB” should be “SB”.
Citation: https://doi.org/10.5194/gmd-2023-30-RC1 -
AC1: 'Reply on RC1', Wenxing Jia, 17 Jul 2023
Response to Referee #1
RE: Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part I: Understanding expressiveness of schemes for different regions from the mechanism perspective
Author(s): Wenxing Jia et al.
In the manuscript “Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part Ⅰ: Understanding expressiveness of schemes for different regions from the mechanism perspective” by Jia et al., the authors select four typical boundary layer parameterization schemes to systematically analyze and evaluate near-surface meteorological parameters, PBL vertical structure, PBLH, and turbulent diffusion in five key regions of China in different seasons. The work can be useful for other researchers to use as a reference when doing simulation studies. I have the following concerns that need to be addressed.
Thank you for your positive comments and valuable suggestions to improve the quality of our manuscript. Based on these comments and suggestions, we have made careful modifications to our pervious draft, and the detailed point-by-point responses are listed below.
Specific comments:
(1) Abstract section: The abstract is too long and needs some reduction.
Re1: Revised as suggested.
(2) Line 204-207: L-band radiosonde observations by the China Meteorological Administration are generally conducted twice a day (08:00 and 20:00 BJT), except for three times a day at individual stations in summer. More details information about the radiosonde observation data are required.
Re2: Revised as suggested.
(3) The convective/unstable boundary layer is an important part of the study of planetary boundary layer. If there is no observation comparison of the daytime PBLH (14:00 BJT), does the author think that the evaluation of PBLH in different seasons in section 3.3 is insufficient.
Re3: Thank you very much for your valuable comments! Indeed, we lack the daily trend analysis of PBLH in this section compared to the conventional meteorological parameters, but we have made a basic comparison analysis of the characteristics of different PBL parameterization schemes to capture the PBLH using the data of these two moments. In the future, we will cooperate with other groups to analyze and discuss the daily variation results of PBLH using Lidar data or encrypted sounding data.
(4) Lines 449-451: Please add the equation for calculating sensible heat flux (HFX) here, so that readers can directly understand the relationship between HFX and Ts-T2, and HFX and Ch.
Re4: Revised as suggested.
(5) Lines 580-581: Add references to previous studies about wind speed, and explain how these results have been accepted by the public.
Re5: Revised as suggested.
(6) Line 591 and 626: The YSU, ACM2 and BL schemes correspond to the revised MM5 near surface scheme and MYJ scheme correspond to another near surface scheme, right? If so, add the near surface scheme corresponding to MYJ scheme in Table 1.
Re6: Revised as suggested.
(7) Lines 817-818: Regarding the criterion of the PBLH about the virtual potential temperature method, it seems the PBLH at dawn and dusk of the studied stations is at the transitional stage of the PBL (08:00 and 20:00 BJT). How can the authors prove that the determined PBLH is accurate and can be used to verify the simulation results of the BL scheme?
Re7: It may be that we did not express it clearly here, we are comparing the PBLH at 08:00 and 20:00, not the daily average of the PBLH. We have made changes in the text and figures.
(8) Line 819 and 822: Please check that the equation number is correct.
Re8: Revised as suggested. Equations 29 and 30 have been modified to equations 15 and 16.
(9) Lines 859-860: For the evaluation of MYJ scheme PBLH, the author uses virtual potential temperature method instead of TKE method. There may be some uncertainties due to different calculation criteria between observation and simulation.
Re9: You are right that there is indeed uncertainty in this comparison, and this sentence (L859-860) has been rewritten so that we should point this out in the manuscript.
(10) As the authors mentioned in the manuscript, there is currently insufficient observational data to calculate PBLH using TKE. What observations should be used to calculate PBLH using TKE? What is the calculation?
Re10: To calculate the PBLH using the TKE method, the perturbation quantities u’, v’ and w’ of the three components of wind speed are needed, and also the data of different heights in the vertical direction are needed so that the TKE of different heights can be calculated, and then the PBLH can be judged according to the threshold value.
(11) Lines 870-871: This is a new attempt to analyze the turbulent diffusion coefficient. The current simulation results have not yet been verified by observations. While it would be strengthen the paper a lot if observational data can be included and analyzed.
Re11: Thank you very much for your acknowledgement that the analysis about turbulent diffusion is currently very scarce, especially from the PBL scheme of the turbulent diffusion mechanism. For now, there are very few observations of turbulent diffusion coefficients, and there is not enough data to be able to analyze them in comparison with the model. We have done some work on the turbulent diffusion of particles with data from one site (Jia et al., 2021a, b; 2022), but the amount of data is still not enough. In the future, if we can cooperate with other groups to get some observation data and do a special issue on turbulent diffusion coefficient, we hope we can get your attention and correction.
Jia, W., and Zhang, X. Impact of modified turbulent diffusion of PM2.5 aerosol in WRF-Chem simulations in eastern China. Atmos. Chem. Phys., 21(22), 16827-16841. doi:10.5194/acp-21-16827-2021, 2021.
Jia, W., Zhang, X.,* Zhang, H.,* and Ren, Y., 2021. Application of turbulent diffusion term of aerosols in mesoscale model, Geophys. Res. Lett., 48, e2021GL093199.
Jia, W., Zhang, X.,* Zhang, H.,* and Ren, Y., 2022. Turbulent transport dissimilarities of particles, momentum and heat. Environ. Res., 211, 113111.
(12) Line 871: “section 3.3.2” should be “section 3.2.2”.
Re12: Revised as suggested.
(13) Figure 14 and 15: “Zhanjiakou” should be changed to “Zhangjiakou”.
Re13: Revised as suggested.
(14) Figure 15: The caption is wrong, not 10-m wind speed and direction.
Re14: We are very sorry, and we have corrected the title of Figure 15.
(15) Figure 16: What do "Ri", “PTv”, "PBLHOBS" and “two methods” stand for? It would be better to state this clearly in the caption.
Re15: Based on your comments, we have added detailed descriptions in the corresponding text and figure 16 captions.
(16) Figure 19: The resolution of the image is too low to distinguish the information shown in the image. And “SCB” should be “SB”.
Re16: In accordance with your comments, we have revised Figure 19 and have checked the entire figure.
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AC1: 'Reply on RC1', Wenxing Jia, 17 Jul 2023
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RC2: 'Comment on gmd-2023-30', Anonymous Referee #2, 05 Jul 2023
This manuscript comprehensively evaluates the performance of four typical boundary layer parameterization schemes (YSU, ACM2, BL and MYJ) over four months (January, April, July and October) in five key regions (NCP, YRD, PRD, SB and NS regions) of China, starting from the mechanism of the parameterization schemes to the optimal solution of the parameterization schemes, and answering almost all the answers that current model users want to know in terms of PBL parameterization schemes. The whole manuscript focuses on the near-surface meteorological parameters in the PBL, including 2-m temperature, 2-m relative humidity, 10-m wind speed and direction, vertical structures of the PBL, PBL height, and turbulence diffusion coefficient, analyzes the reasons for the differences between different PBL parameterization schemes, discusses the differences between PBL parameterization schemes and observations, and gives suggestions for the optimal solutions of PBL parameterization schemes. I do have some comments, which I believe should be addressed before the manuscript is considered for publication:
- The abstract section is a bit too long, the article is rich in content and there are many results to show, so you need to take it and streamline the abstract.
- Why these four boundary layer parameterization schemes were chosen, and whether the corresponding explanatory notes can be given in the appropriate places?
- What was the basis for the selection of sounding sites in each region?
- The second part of the manuscript should describe the topographical and regional characteristics of the five regions and why they were chosen.
- The analysis of this part of L423-498 is very clear, but the part of L499-522 is a little bit messy and needs to be reorganized, therefore, there is a leading sentence to make the idea clearer.
- In the section 3.4, are there any observations of turbulent diffusion for the relevant comparison work?
- In fact, there are many articles about PBL parameterization schemes, most of them are more or less the same. This manuscript has analyzed and evaluated the PBL parameterization scheme very comprehensively, which is of great reference to the readers. Could you add a paragraph at the end of the manuscript with thoughts and suggestions on the PBL parameterization scheme?
Minor issues:
- Table 1, A near surface layer parameterization scheme is missing, because MYJ can only couple Eta near surface layer scheme.
- L258, “Rib” should be changed to “Ribcr”.
- L331-334, Eq. (13a), Eq. (13b) and Eq. (13c) switch the order and correspond to the previous ones.
- L391, “structure” should be changed to “structures”.
- L400, “orange dots” should be changed to “purple dots” in Figure 1.
- L449-451, The formula of HFX should be given out.
- L506, here, should also include a part of Shandong Province, “Hebei province” should be changed to “Hebei and Shandong provinces”.
- L523-524, this sentence needs to be rewritten.
- L560-561, according to Figures 2-6 and supplement, this conclusion should be directed especially to winter, i.e., October and January.
- L614, “WS10” should be changed to “WS10”.
- L816, “planetary boundary layer height” should be deleted.
- L819, here, it is not these two equations, it should be equations (15) and (16).
- L822, “Eq. 29” should be changed to “Eq. (15)”.
- L837-839, what is the reason for the PBLH simulated by the BL scheme is better than the other three schemes, and the poor simulation results of the MYJ scheme?
- L872, “turbulent diffusion coefficient” should be deleted.
- L875, “structure” should be changed to “structures”.
- L888, lack of figure citation, and figure 18 is only for the NCP region.
- L904-928, Add some references as supporting notes.
- L935-942, the “SCB” in Figure 19 should be changed to “SB”.
- L1021, “planetary boundary layer” should be changed to “PBL”.
- L1073, “vertical distribution of PBL” should be changed to “PBL vertical structures”.
- There are more figures, which need to be provided in high resolution (especially Figure 19), as well as double-checking the figure title of each figure.
- The citation format of references in the manuscript needs to be standardized, especially in the introduction.
Citation: https://doi.org/10.5194/gmd-2023-30-RC2 -
AC2: 'Reply on RC2', Wenxing Jia, 17 Jul 2023
Response to Referee #2
RE: Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part I: Understanding expressiveness of schemes for different regions from the mechanism perspective
Author(s): Wenxing Jia et al.
This manuscript comprehensively evaluates the performance of four typical boundary layer parameterization schemes (YSU, ACM2, BL and MYJ) over four months (January, April, July and October) in five key regions (NCP, YRD, PRD, SB and NS regions) of China, starting from the mechanism of the parameterization schemes to the optimal solution of the parameterization schemes, and answering almost all the answers that current model users want to know in terms of PBL parameterization schemes. The whole manuscript focuses on the near-surface meteorological parameters in the PBL, including 2-m temperature, 2-m relative humidity, 10-m wind speed and direction, vertical structures of the PBL, PBL height, and turbulence diffusion coefficient, analyzes the reasons for the differences between different PBL parameterization schemes, discusses the differences between PBL parameterization schemes and observations, and gives suggestions for the optimal solutions of PBL parameterization schemes. I do have some comments, which I believe should be addressed before the manuscript is considered for publication:
Thank you for your positive comments and valuable suggestions to improve the quality of our manuscript. Based on these comments and suggestions, we have made careful modifications to our pervious draft, and the detailed point-by-point responses are listed below.
Specific comments:
- The abstract section is a bit too long, the article is rich in content and there are many results to show, so you need to take it and streamline the abstract.
Re1: Revised as suggested.
- Why these four boundary layer parameterization schemes were chosen, and whether the corresponding explanatory notes can be given in the appropriate places?
Re2: There are three categories of PBL parameterization schemes, nonlocal, local and hybrid. Considering that each category of parameterization schemes should be covered, for each category, a typical parameterization scheme in that category is selected.
- What was the basis for the selection of sounding sites in each region?
Re3: Four sounding stations have been selected for each region, including different underlying surface conditions as much as possible.
- The second part of the manuscript should describe the topographical and regional characteristics of the five regions and why they were chosen.
Re4: Revised as suggested.
- The analysis of this part of L423-498 is very clear, but the part of L499-522 is a little bit messy and needs to be reorganized, therefore, there is a leading sentence to make the idea clearer.
Re5: Revised as suggested.
- In the section 3.4, are there any observations of turbulent diffusion for the relevant comparison work?
Re6: Currently, observations of turbulent diffusion are still scarce, especially for multilayer turbulence observations throughout the vertical direction within the PBL.
- In fact, there are many articles about PBL parameterization schemes, most of them are more or less the same. This manuscript has analyzed and evaluated the PBL parameterization scheme very comprehensively, which is of great reference to the readers. Could you add a paragraph at the end of the manuscript with thoughts and suggestions on the PBL parameterization scheme?
Re7: Revised as suggested. “The PBL parameterization scheme, as the most critical parameterization process within the PBL in the model, has been well proposed and developed by previous generations, but the development has been slower in recent years, few new theories have been proposed and almost no new schemes have been put into the model or the existing schemes have rarely been improved. Most of the previous studies have evaluated the PBL parameterization scheme, but many of them focus on a particular case in a certain region and lack of universality. This study makes up for this deficiency and provides a comprehensive discussion on the evaluation and uncertainty analysis of the PBL parameterization scheme, hoping to give some reference to the model users. The future development of the PBL parameterization scheme needs to start from the theoretical mechanism, go deeper into the PBL parameterization scheme, and have a deeper understanding of the PBL parameterization, even if it is only for one scheme, or the improvement of one parameter. And for China's self-developed GRAPES model, the introduction and improvement of PBL parameterization schemes need to be selected, rather than a brain to write all the schemes, in fact, many schemes are almost not measured and used.”
Minor issues:
- Table 1, A near surface layer parameterization scheme is missing, because MYJ can only couple Eta near surface layer scheme.
Re1: Revised as suggested.
- L258, “Rib” should be changed to “Ribcr”.
Re2: Revised as suggested.
- L331-334, Eq. (13a), Eq. (13b) and Eq. (13c) switch the order and correspond to the previous ones.
Re3: Revised as suggested.
- L391, “structure” should be changed to “structures”.
Re4: Revised as suggested.
- L400, “orange dots” should be changed to “purple dots” in Figure 1.
Re5: Revised as suggested.
- L449-451, The formula of HFX should be given out.
Re6: Revised as suggested.
- L506, here, should also include a part of Shandong Province, “Hebei province” should be changed to “Hebei and Shandong provinces”.
Re7: Revised as suggested.
- L523-524, this sentence needs to be rewritten.
Re8: Revised as suggested.
- L560-561, according to Figures 2-6 and supplement, this conclusion should be directed especially to winter, i.e., October and January.
Re9: Revised as suggested.
- L614, “WS10” should be changed to “WS10”.
Re10: Revised as suggested.
- L816, “planetary boundary layer height” should be deleted.
Re11: Revised as suggested.
- L819, here, it is not these two equations, it should be equations (15) and (16).
Re12: Revised as suggested.
- L822, “Eq. 29” should be changed to “Eq. (15)”.
Re13: Revised as suggested.
- L837-839, what is the reason for the PBLH simulated by the BL scheme is better than the other three schemes, and the poor simulation results of the MYJ scheme?
Re14: This is because the BL scheme calculates the PBLH by the virtual potential temperature method, and the model gives the best simulation results for temperature.
- L872, “turbulent diffusion coefficient” should be deleted.
Re15: Revised as suggested.
- L875, “structure” should be changed to “structures”.
Re16: Revised as suggested.
- L888, lack of figure citation, and figure 18 is only for the NCP region.
Re17: Revised as suggested.
- L904-928, Add some references as supporting notes.
Re18: Revised as suggested.
- L935-942, the “SCB” in Figure 19 should be changed to “SB”.
Re19: Revised as suggested.
- L1021, “planetary boundary layer” should be changed to “PBL”.
Re20: Revised as suggested.
- L1073, “vertical distribution of PBL” should be changed to “PBL vertical structures”.
Re21: Revised as suggested.
- There are more figures, which need to be provided in high resolution (especially Figure 19), as well as double-checking the figure title of each figure.
Re22: Revised as suggested.
- The citation format of references in the manuscript needs to be standardized, especially in the introduction.
Re23: Revised as suggested.
Status: closed
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RC1: 'Comment on gmd-2023-30', Anonymous Referee #1, 28 May 2023
In the manuscript “Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part Ⅰ: Understanding expressiveness of schemes for different regions from the mechanism perspective” by Jia et al., the authors select four typical boundary layer parameterization schemes to systematically analyze and evaluate near-surface meteorological parameters, PBL vertical structure, PBLH, and turbulent diffusion in five key regions of China in different seasons. The work can be useful for other researchers to use as a reference when doing simulation studies. I have the following concerns that need to be addressed.
Specific comments:
(1) Abstract section: The abstract is too long and needs some reduction.
(2) Line 204-207: L-band radiosonde observations by the China Meteorological Administration are generally conducted twice a day (08:00 and 20:00 BJT), except for three times a day at individual stations in summer. More details information about the radiosonde observation data are required.
(3) The convective/unstable boundary layer is an important part of the study of planetary boundary layer. If there is no observation comparison of the daytime PBLH (14:00 BJT), does the author think that the evaluation of PBLH in different seasons in section 3.3 is insufficient.
(4) Lines 449-451: Please add the equation for calculating sensible heat flux (HFX) here, so that readers can directly understand the relationship between HFX and Ts-T2, and HFX and Ch.
(5) Lines 580-581: Add references to previous studies about wind speed, and explain how these results have been accepted by the public.
(6) Line 591 and 626: The YSU, ACM2 and BL schemes correspond to the revised MM5 near surface scheme and MYJ scheme correspond to another near surface scheme, right? If so, add the near surface scheme corresponding to MYJ scheme in Table 1.
(7) Lines 817-818: Regarding the criterion of the PBLH about the virtual potential temperature method, it seems the PBLH at dawn and dusk of the studied stations is at the transitional stage of the PBL (08:00 and 20:00 BJT). How can the authors prove that the determined PBLH is accurate and can be used to verify the simulation results of the BL scheme?
(8) Line 819 and 822: Please check that the equation number is correct.
(9) Lines 859-860: For the evaluation of MYJ scheme PBLH, the author uses virtual potential temperature method instead of TKE method. There may be some uncertainties due to different calculation criteria between observation and simulation.
(10) As the authors mentioned in the manuscript, there is currently insufficient observational data to calculate PBLH using TKE. What observations should be used to calculate PBLH using TKE? What is the calculation?
(11) Lines 870-871: This is a new attempt to analyze the turbulent diffusion coefficient. The current simulation results have not yet been verified by observations. While it would be strengthen the paper a lot if observational data can be included and analyzed.
(12) Line 871: “section 3.3.2” should be “section 3.2.2”.
(13) Figure 14 and 15: “Zhanjiakou” should be changed to “Zhangjiakou”.
(14) Figure 15: The caption is wrong, not 10-m wind speed and direction.
(15) Figure 16: What do "Ri", “PTv”, "PBLHOBS" and “two methods” stand for? It would be better to state this clearly in the caption.
(16) Figure 19: The resolution of the image is too low to distinguish the information shown in the image. And “SCB” should be “SB”.
Citation: https://doi.org/10.5194/gmd-2023-30-RC1 -
AC1: 'Reply on RC1', Wenxing Jia, 17 Jul 2023
Response to Referee #1
RE: Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part I: Understanding expressiveness of schemes for different regions from the mechanism perspective
Author(s): Wenxing Jia et al.
In the manuscript “Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part Ⅰ: Understanding expressiveness of schemes for different regions from the mechanism perspective” by Jia et al., the authors select four typical boundary layer parameterization schemes to systematically analyze and evaluate near-surface meteorological parameters, PBL vertical structure, PBLH, and turbulent diffusion in five key regions of China in different seasons. The work can be useful for other researchers to use as a reference when doing simulation studies. I have the following concerns that need to be addressed.
Thank you for your positive comments and valuable suggestions to improve the quality of our manuscript. Based on these comments and suggestions, we have made careful modifications to our pervious draft, and the detailed point-by-point responses are listed below.
Specific comments:
(1) Abstract section: The abstract is too long and needs some reduction.
Re1: Revised as suggested.
(2) Line 204-207: L-band radiosonde observations by the China Meteorological Administration are generally conducted twice a day (08:00 and 20:00 BJT), except for three times a day at individual stations in summer. More details information about the radiosonde observation data are required.
Re2: Revised as suggested.
(3) The convective/unstable boundary layer is an important part of the study of planetary boundary layer. If there is no observation comparison of the daytime PBLH (14:00 BJT), does the author think that the evaluation of PBLH in different seasons in section 3.3 is insufficient.
Re3: Thank you very much for your valuable comments! Indeed, we lack the daily trend analysis of PBLH in this section compared to the conventional meteorological parameters, but we have made a basic comparison analysis of the characteristics of different PBL parameterization schemes to capture the PBLH using the data of these two moments. In the future, we will cooperate with other groups to analyze and discuss the daily variation results of PBLH using Lidar data or encrypted sounding data.
(4) Lines 449-451: Please add the equation for calculating sensible heat flux (HFX) here, so that readers can directly understand the relationship between HFX and Ts-T2, and HFX and Ch.
Re4: Revised as suggested.
(5) Lines 580-581: Add references to previous studies about wind speed, and explain how these results have been accepted by the public.
Re5: Revised as suggested.
(6) Line 591 and 626: The YSU, ACM2 and BL schemes correspond to the revised MM5 near surface scheme and MYJ scheme correspond to another near surface scheme, right? If so, add the near surface scheme corresponding to MYJ scheme in Table 1.
Re6: Revised as suggested.
(7) Lines 817-818: Regarding the criterion of the PBLH about the virtual potential temperature method, it seems the PBLH at dawn and dusk of the studied stations is at the transitional stage of the PBL (08:00 and 20:00 BJT). How can the authors prove that the determined PBLH is accurate and can be used to verify the simulation results of the BL scheme?
Re7: It may be that we did not express it clearly here, we are comparing the PBLH at 08:00 and 20:00, not the daily average of the PBLH. We have made changes in the text and figures.
(8) Line 819 and 822: Please check that the equation number is correct.
Re8: Revised as suggested. Equations 29 and 30 have been modified to equations 15 and 16.
(9) Lines 859-860: For the evaluation of MYJ scheme PBLH, the author uses virtual potential temperature method instead of TKE method. There may be some uncertainties due to different calculation criteria between observation and simulation.
Re9: You are right that there is indeed uncertainty in this comparison, and this sentence (L859-860) has been rewritten so that we should point this out in the manuscript.
(10) As the authors mentioned in the manuscript, there is currently insufficient observational data to calculate PBLH using TKE. What observations should be used to calculate PBLH using TKE? What is the calculation?
Re10: To calculate the PBLH using the TKE method, the perturbation quantities u’, v’ and w’ of the three components of wind speed are needed, and also the data of different heights in the vertical direction are needed so that the TKE of different heights can be calculated, and then the PBLH can be judged according to the threshold value.
(11) Lines 870-871: This is a new attempt to analyze the turbulent diffusion coefficient. The current simulation results have not yet been verified by observations. While it would be strengthen the paper a lot if observational data can be included and analyzed.
Re11: Thank you very much for your acknowledgement that the analysis about turbulent diffusion is currently very scarce, especially from the PBL scheme of the turbulent diffusion mechanism. For now, there are very few observations of turbulent diffusion coefficients, and there is not enough data to be able to analyze them in comparison with the model. We have done some work on the turbulent diffusion of particles with data from one site (Jia et al., 2021a, b; 2022), but the amount of data is still not enough. In the future, if we can cooperate with other groups to get some observation data and do a special issue on turbulent diffusion coefficient, we hope we can get your attention and correction.
Jia, W., and Zhang, X. Impact of modified turbulent diffusion of PM2.5 aerosol in WRF-Chem simulations in eastern China. Atmos. Chem. Phys., 21(22), 16827-16841. doi:10.5194/acp-21-16827-2021, 2021.
Jia, W., Zhang, X.,* Zhang, H.,* and Ren, Y., 2021. Application of turbulent diffusion term of aerosols in mesoscale model, Geophys. Res. Lett., 48, e2021GL093199.
Jia, W., Zhang, X.,* Zhang, H.,* and Ren, Y., 2022. Turbulent transport dissimilarities of particles, momentum and heat. Environ. Res., 211, 113111.
(12) Line 871: “section 3.3.2” should be “section 3.2.2”.
Re12: Revised as suggested.
(13) Figure 14 and 15: “Zhanjiakou” should be changed to “Zhangjiakou”.
Re13: Revised as suggested.
(14) Figure 15: The caption is wrong, not 10-m wind speed and direction.
Re14: We are very sorry, and we have corrected the title of Figure 15.
(15) Figure 16: What do "Ri", “PTv”, "PBLHOBS" and “two methods” stand for? It would be better to state this clearly in the caption.
Re15: Based on your comments, we have added detailed descriptions in the corresponding text and figure 16 captions.
(16) Figure 19: The resolution of the image is too low to distinguish the information shown in the image. And “SCB” should be “SB”.
Re16: In accordance with your comments, we have revised Figure 19 and have checked the entire figure.
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AC1: 'Reply on RC1', Wenxing Jia, 17 Jul 2023
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RC2: 'Comment on gmd-2023-30', Anonymous Referee #2, 05 Jul 2023
This manuscript comprehensively evaluates the performance of four typical boundary layer parameterization schemes (YSU, ACM2, BL and MYJ) over four months (January, April, July and October) in five key regions (NCP, YRD, PRD, SB and NS regions) of China, starting from the mechanism of the parameterization schemes to the optimal solution of the parameterization schemes, and answering almost all the answers that current model users want to know in terms of PBL parameterization schemes. The whole manuscript focuses on the near-surface meteorological parameters in the PBL, including 2-m temperature, 2-m relative humidity, 10-m wind speed and direction, vertical structures of the PBL, PBL height, and turbulence diffusion coefficient, analyzes the reasons for the differences between different PBL parameterization schemes, discusses the differences between PBL parameterization schemes and observations, and gives suggestions for the optimal solutions of PBL parameterization schemes. I do have some comments, which I believe should be addressed before the manuscript is considered for publication:
- The abstract section is a bit too long, the article is rich in content and there are many results to show, so you need to take it and streamline the abstract.
- Why these four boundary layer parameterization schemes were chosen, and whether the corresponding explanatory notes can be given in the appropriate places?
- What was the basis for the selection of sounding sites in each region?
- The second part of the manuscript should describe the topographical and regional characteristics of the five regions and why they were chosen.
- The analysis of this part of L423-498 is very clear, but the part of L499-522 is a little bit messy and needs to be reorganized, therefore, there is a leading sentence to make the idea clearer.
- In the section 3.4, are there any observations of turbulent diffusion for the relevant comparison work?
- In fact, there are many articles about PBL parameterization schemes, most of them are more or less the same. This manuscript has analyzed and evaluated the PBL parameterization scheme very comprehensively, which is of great reference to the readers. Could you add a paragraph at the end of the manuscript with thoughts and suggestions on the PBL parameterization scheme?
Minor issues:
- Table 1, A near surface layer parameterization scheme is missing, because MYJ can only couple Eta near surface layer scheme.
- L258, “Rib” should be changed to “Ribcr”.
- L331-334, Eq. (13a), Eq. (13b) and Eq. (13c) switch the order and correspond to the previous ones.
- L391, “structure” should be changed to “structures”.
- L400, “orange dots” should be changed to “purple dots” in Figure 1.
- L449-451, The formula of HFX should be given out.
- L506, here, should also include a part of Shandong Province, “Hebei province” should be changed to “Hebei and Shandong provinces”.
- L523-524, this sentence needs to be rewritten.
- L560-561, according to Figures 2-6 and supplement, this conclusion should be directed especially to winter, i.e., October and January.
- L614, “WS10” should be changed to “WS10”.
- L816, “planetary boundary layer height” should be deleted.
- L819, here, it is not these two equations, it should be equations (15) and (16).
- L822, “Eq. 29” should be changed to “Eq. (15)”.
- L837-839, what is the reason for the PBLH simulated by the BL scheme is better than the other three schemes, and the poor simulation results of the MYJ scheme?
- L872, “turbulent diffusion coefficient” should be deleted.
- L875, “structure” should be changed to “structures”.
- L888, lack of figure citation, and figure 18 is only for the NCP region.
- L904-928, Add some references as supporting notes.
- L935-942, the “SCB” in Figure 19 should be changed to “SB”.
- L1021, “planetary boundary layer” should be changed to “PBL”.
- L1073, “vertical distribution of PBL” should be changed to “PBL vertical structures”.
- There are more figures, which need to be provided in high resolution (especially Figure 19), as well as double-checking the figure title of each figure.
- The citation format of references in the manuscript needs to be standardized, especially in the introduction.
Citation: https://doi.org/10.5194/gmd-2023-30-RC2 -
AC2: 'Reply on RC2', Wenxing Jia, 17 Jul 2023
Response to Referee #2
RE: Comprehensive evaluation of typical planetary boundary layer (PBL) parameterization schemes in China. Part I: Understanding expressiveness of schemes for different regions from the mechanism perspective
Author(s): Wenxing Jia et al.
This manuscript comprehensively evaluates the performance of four typical boundary layer parameterization schemes (YSU, ACM2, BL and MYJ) over four months (January, April, July and October) in five key regions (NCP, YRD, PRD, SB and NS regions) of China, starting from the mechanism of the parameterization schemes to the optimal solution of the parameterization schemes, and answering almost all the answers that current model users want to know in terms of PBL parameterization schemes. The whole manuscript focuses on the near-surface meteorological parameters in the PBL, including 2-m temperature, 2-m relative humidity, 10-m wind speed and direction, vertical structures of the PBL, PBL height, and turbulence diffusion coefficient, analyzes the reasons for the differences between different PBL parameterization schemes, discusses the differences between PBL parameterization schemes and observations, and gives suggestions for the optimal solutions of PBL parameterization schemes. I do have some comments, which I believe should be addressed before the manuscript is considered for publication:
Thank you for your positive comments and valuable suggestions to improve the quality of our manuscript. Based on these comments and suggestions, we have made careful modifications to our pervious draft, and the detailed point-by-point responses are listed below.
Specific comments:
- The abstract section is a bit too long, the article is rich in content and there are many results to show, so you need to take it and streamline the abstract.
Re1: Revised as suggested.
- Why these four boundary layer parameterization schemes were chosen, and whether the corresponding explanatory notes can be given in the appropriate places?
Re2: There are three categories of PBL parameterization schemes, nonlocal, local and hybrid. Considering that each category of parameterization schemes should be covered, for each category, a typical parameterization scheme in that category is selected.
- What was the basis for the selection of sounding sites in each region?
Re3: Four sounding stations have been selected for each region, including different underlying surface conditions as much as possible.
- The second part of the manuscript should describe the topographical and regional characteristics of the five regions and why they were chosen.
Re4: Revised as suggested.
- The analysis of this part of L423-498 is very clear, but the part of L499-522 is a little bit messy and needs to be reorganized, therefore, there is a leading sentence to make the idea clearer.
Re5: Revised as suggested.
- In the section 3.4, are there any observations of turbulent diffusion for the relevant comparison work?
Re6: Currently, observations of turbulent diffusion are still scarce, especially for multilayer turbulence observations throughout the vertical direction within the PBL.
- In fact, there are many articles about PBL parameterization schemes, most of them are more or less the same. This manuscript has analyzed and evaluated the PBL parameterization scheme very comprehensively, which is of great reference to the readers. Could you add a paragraph at the end of the manuscript with thoughts and suggestions on the PBL parameterization scheme?
Re7: Revised as suggested. “The PBL parameterization scheme, as the most critical parameterization process within the PBL in the model, has been well proposed and developed by previous generations, but the development has been slower in recent years, few new theories have been proposed and almost no new schemes have been put into the model or the existing schemes have rarely been improved. Most of the previous studies have evaluated the PBL parameterization scheme, but many of them focus on a particular case in a certain region and lack of universality. This study makes up for this deficiency and provides a comprehensive discussion on the evaluation and uncertainty analysis of the PBL parameterization scheme, hoping to give some reference to the model users. The future development of the PBL parameterization scheme needs to start from the theoretical mechanism, go deeper into the PBL parameterization scheme, and have a deeper understanding of the PBL parameterization, even if it is only for one scheme, or the improvement of one parameter. And for China's self-developed GRAPES model, the introduction and improvement of PBL parameterization schemes need to be selected, rather than a brain to write all the schemes, in fact, many schemes are almost not measured and used.”
Minor issues:
- Table 1, A near surface layer parameterization scheme is missing, because MYJ can only couple Eta near surface layer scheme.
Re1: Revised as suggested.
- L258, “Rib” should be changed to “Ribcr”.
Re2: Revised as suggested.
- L331-334, Eq. (13a), Eq. (13b) and Eq. (13c) switch the order and correspond to the previous ones.
Re3: Revised as suggested.
- L391, “structure” should be changed to “structures”.
Re4: Revised as suggested.
- L400, “orange dots” should be changed to “purple dots” in Figure 1.
Re5: Revised as suggested.
- L449-451, The formula of HFX should be given out.
Re6: Revised as suggested.
- L506, here, should also include a part of Shandong Province, “Hebei province” should be changed to “Hebei and Shandong provinces”.
Re7: Revised as suggested.
- L523-524, this sentence needs to be rewritten.
Re8: Revised as suggested.
- L560-561, according to Figures 2-6 and supplement, this conclusion should be directed especially to winter, i.e., October and January.
Re9: Revised as suggested.
- L614, “WS10” should be changed to “WS10”.
Re10: Revised as suggested.
- L816, “planetary boundary layer height” should be deleted.
Re11: Revised as suggested.
- L819, here, it is not these two equations, it should be equations (15) and (16).
Re12: Revised as suggested.
- L822, “Eq. 29” should be changed to “Eq. (15)”.
Re13: Revised as suggested.
- L837-839, what is the reason for the PBLH simulated by the BL scheme is better than the other three schemes, and the poor simulation results of the MYJ scheme?
Re14: This is because the BL scheme calculates the PBLH by the virtual potential temperature method, and the model gives the best simulation results for temperature.
- L872, “turbulent diffusion coefficient” should be deleted.
Re15: Revised as suggested.
- L875, “structure” should be changed to “structures”.
Re16: Revised as suggested.
- L888, lack of figure citation, and figure 18 is only for the NCP region.
Re17: Revised as suggested.
- L904-928, Add some references as supporting notes.
Re18: Revised as suggested.
- L935-942, the “SCB” in Figure 19 should be changed to “SB”.
Re19: Revised as suggested.
- L1021, “planetary boundary layer” should be changed to “PBL”.
Re20: Revised as suggested.
- L1073, “vertical distribution of PBL” should be changed to “PBL vertical structures”.
Re21: Revised as suggested.
- There are more figures, which need to be provided in high resolution (especially Figure 19), as well as double-checking the figure title of each figure.
Re22: Revised as suggested.
- The citation format of references in the manuscript needs to be standardized, especially in the introduction.
Re23: Revised as suggested.
Wenxing Jia et al.
Wenxing Jia et al.
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