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Artikel ; Online: Commentary on: core decompression combined with platelet-rich plasma-augmented bone grafting for femur head necrosis: a systematic review and meta-analysis.

Ye, Baisheng / Li, Wei / Meng, Shilong / Shi, Xiaolin

International journal of surgery (London, England)

2024

Sprache	Englisch
Erscheinungsdatum	2024-04-23
Erscheinungsland	United States
Dokumenttyp	Journal Article
ZDB-ID	2212038-5
ISSN	1743-9159 ; 1743-9191
ISSN (online)	1743-9159
ISSN	1743-9191
DOI	10.1097/JS9.0000000000001492
Datenquelle	MEDical Literature Analysis and Retrieval System OnLINE

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Artikel ; Online: A commentary on "causal effects of gut microbiota on renal tumor: a mendelian randomization study".

Huang, Zhen / Ye, Baisheng / Li, Wei / Shi, Xiaolin

International journal of surgery (London, England)

2024

Sprache	Englisch
Erscheinungsdatum	2024-05-08
Erscheinungsland	United States
Dokumenttyp	Journal Article
ZDB-ID	2212038-5
ISSN	1743-9159 ; 1743-9191
ISSN (online)	1743-9159
ISSN	1743-9191
DOI	10.1097/JS9.0000000000001567
Datenquelle	MEDical Literature Analysis and Retrieval System OnLINE

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Artikel ; Online: Commentary on: Immediate mobilization after repair of Achilles tendon rupture may increase the incidence of re-rupture: a systematic review and meta-analysis of randomized controlled trials.

Meng, Shilong / Zhang, Xu / Ye, Baisheng / Shi, Xiaolin / Liu, Kang

International journal of surgery (London, England)

2024

Sprache	Englisch
Erscheinungsdatum	2024-04-22
Erscheinungsland	United States
Dokumenttyp	Journal Article
ZDB-ID	2212038-5
ISSN	1743-9159 ; 1743-9191
ISSN (online)	1743-9159
ISSN	1743-9191
DOI	10.1097/JS9.0000000000001490
Datenquelle	MEDical Literature Analysis and Retrieval System OnLINE

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Artikel ; Online: Effects of kidney tonic herbs for primary osteoporosis: A systematic review and meta-analysis.

Li, Wei / Ye, Baisheng / Huang, Zhen / Zhou, Hang / Feng, Jie / Chen, Qi / Huang, Hai / Meng, Shilong / Qie, Fengqing / Shi, Xiaolin

Medicine

2023 Band 102, Heft 43, Seite(n) e35061

Abstract: Background: Primary osteoporosis (POP) is one of the most common orthopedic conditions with a high risk of fractures. Effective treatment of POP is crucial for reducing disability rates and improving quality of life. Kidney tonic therapy is a classical ... ...

Abstract	Background: Primary osteoporosis (POP) is one of the most common orthopedic conditions with a high risk of fractures. Effective treatment of POP is crucial for reducing disability rates and improving quality of life. Kidney tonic therapy is a classical traditional Chinese medicine approach for treating POP. This study aims to provide a comprehensive and reliable assessment of the clinical evidence of kidney tonic herbs (KTH) in treating POP patients. Methods: An extensive literature search was conducted in 8 electronic databases from their inception through September 30, 2022, to evaluate the efficacy and safety of KTH for POP. We included 43 randomized controlled trials with 4349 participants. The qualified studies will be chosen and evaluated separately by 2 researchers. The primary outcome measure was bone mineral density (BMD) of lumbar. RevMan 5.3 and Stata 16 were used to carry out the meta-analyses. Results: Our meta-analysis showed 29 studies with significantly increased lumbar BMD (mean difference [MD] = 0.06; 95% confidence interval [CI]; I2 = 98%, P = .003), 18 studies with noticeably higher femoral neck BMD (MD = 0.08; 95% CI; I2 = 98%, P = .0005), 6 studies with significantly increased femoral trochanter BMD (MD = 0.10; 95% CI; I2 = 97%, P = .002), 4 studies with noticeably higher ward's triangle BMD (MD = 0.13; 95% CI; I2 = 100%, P = .04), and 3 studies with noticeably higher distal radius BMD (MD = 0.06; 95% CI; I2 = 86%, P = .009). One study showed 12 falls and 8 fallers in the intervention group, 28 falls and 17 fallers in the control group at 36 months. 3 studies showed a significant difference in fracture incidence between the intervention group and the control group (95% CI: 0.15-0.81; I2 = 0%, P = .01). Additionally, the meta-analysis demonstrated that KTH offered superior pain relief (8 trials, n = 980; 95% CI: -1.05 to -0.74; I2 = 94%, P < .00001). Besides, KTH found no serious harmful effects. Discussion: KTH may increase BMD and decrease the likelihood of fractures in POP patients. However, further research is necessary to investigate the effectiveness of KTH in reducing falls and fractures.
Mesh-Begriff(e)	Humans ; Osteoporosis/drug therapy ; Quality of Life ; Bone Density ; Fractures, Bone ; Kidney
Sprache	Englisch
Erscheinungsdatum	2023-11-01
Erscheinungsland	United States
Dokumenttyp	Meta-Analysis ; Systematic Review ; Journal Article
ZDB-ID	80184-7
ISSN	1536-5964 ; 0025-7974
ISSN (online)	1536-5964
ISSN	0025-7974
DOI	10.1097/MD.0000000000035061
Datenquelle	MEDical Literature Analysis and Retrieval System OnLINE

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Artikel: Characteristics of melt water discharge in the Glacier No. 1 basin, headwater of Urumqi River

Mingjie, Gao / Han Tianding / Jiao Keqin / Ye Baisheng

Journal of hydrology. 2013 May 10, v. 489

2013

Abstract: Characteristics of the daily melt water discharge cycle and the relation between melt water discharge, air temperature, and precipitation are analyzed based on observation data during 2001–2005 in the Glacier No. 1 basin at the headwater of the Urumqi ... ...

Abstract	Characteristics of the daily melt water discharge cycle and the relation between melt water discharge, air temperature, and precipitation are analyzed based on observation data during 2001–2005 in the Glacier No. 1 basin at the headwater of the Urumqi River, Tianshan Mountains (hereafter, Glacier No. 1). The results indicate that the daytime and nighttime discharges were less during the preliminary stage of melting in May, and became strong following the ablation period (July–August). The daytime and nighttime discharges in the same month varied year-over-year, and the daily discharge cycles in different months of the summer were dissimilar.The mean daytime/nighttime discharges were somewhat related to the mean nighttime air temperature (Tn), but were not significantly related to the amount of precipitation. In the daily cycle of average discharges in the summer months during 2001–2005, the maximum discharges occurred in the afternoons and evenings, and the minimum discharges occurred in the mornings. The daily discharge peaks lagged behind the time of maximum melting (maximum air temperature) on selected clear-weather days in different months in different years. This was related to the melt water flow distance inside and underneath the glacier and the structure of the internal drainage net, and may also have been influenced by the weather prior to and after the observed consecutive clear-weather days.The monthly mean daytime discharge was generally greater than the nighttime discharge, primarily because cloudy and rainy weather and lower air temperatures led to less melt water, and precipitation could not make up the loss of discharge from melt water. Daytime melt water contributed only slightly to nighttime discharge due to the short time lag caused by melt water flow distance.
Schlagwörter	air temperature ; basins ; glaciers ; hydrologic cycle ; internal drainage ; melting ; mountains ; rivers ; summer ; water flow ; weather
Sprache	Englisch
Erscheinungsverlauf	2013-0510
Umfang	p. 180-188.
Erscheinungsort	Elsevier B.V.
Dokumenttyp	Artikel
ZDB-ID	1473173-3
ISSN	0022-1694
ISSN	0022-1694
DOI	10.1016/j.jhydrol.2013.03.013
Datenquelle	NAL Katalog (AGRICOLA)

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Artikel: Modeling the runoff and glacier mass balance in a small watershed on the Central Tibetan Plateau, China, from 1955 to 2008

Gao, Hongkai / He, Xiaobo / Ye, Baisheng / Pu, Jianchen

Hydrological processes. 2012 May 30, v. 26, no. 11

2012

Abstract: The glaciers on Tibetan Plateau play an important role in the catchment hydrology of this region. However, our knowledge with respect to water circulation in this remote area is scarce. In this study, the HBV light model, which adopts the degree‐day ... ...

Abstract	The glaciers on Tibetan Plateau play an important role in the catchment hydrology of this region. However, our knowledge with respect to water circulation in this remote area is scarce. In this study, the HBV light model, which adopts the degree‐day model for glacial melting, was employed to simulate the total runoff, the glacier runoff and glacier mass balance (GMB) of the Dongkemadi River Basin (DRB) at the headwater of the Yangtze River on the Tibetan Plateau, China. Firstly, the daily temperature and precipitation of the DRB from 1955 to 2008 were obtained by statistical methods, based on daily meteorological data observed in the DRB (2005–2008) and recorded by four national meteorological stations near the DRB (1955–2008). Secondly, we used 4‐year daily air temperature, precipitation, runoff depth and monthly evaporation, which were observed in the DRB, as input to obtain a set of proper parameters. Then, the annual runoff, the glacier runoff and GMB (1955–2008) were calculated using the HBV model driven by interpolated meteorological data. The calculated GMB fits well with the observed results. At last, using the temperature and precipitation predicted by climate models, we predicted the changes of runoff depth and GMB of the DRB in the next 40 years. Under all climate‐change scenarios, annual glacier runoff shows a significant increase due to intensified ice melting.
Schlagwörter	air temperature ; atmospheric precipitation ; climate models ; evaporation ; glaciers ; hydrologic models ; melting ; meteorological data ; plateaus ; runoff ; statistical analysis ; water flow ; watershed hydrology ; watersheds ; China ; Yangtze River
Sprache	Englisch
Erscheinungsverlauf	2012-0530
Umfang	p. 1593-1603.
Erscheinungsort	John Wiley & Sons, Ltd
Dokumenttyp	Artikel
ZDB-ID	1479953-4
ISSN	1099-1085 ; 0885-6087
ISSN (online)	1099-1085
ISSN	0885-6087
DOI	10.1002/hyp.8256
Datenquelle	NAL Katalog (AGRICOLA)

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Artikel: Responses of Alpine Grassland to Climate Warming and Permafrost Thawing in Two Basins with Different Precipitation Regimes on the Qinghai-Tibetan Plateaus

Zhou, Zhaoye / Chen Jianjun / Ding Yongjian / Sheng Yu / Wang Genxu / Ye Baisheng / Yi Shuhua

Arctic, antarctic, and alpine research. 2015 Feb., v. 47, no. 1

2015

Abstract: Alpine grassland and permafrost occupy about two thirds and one half of the total area of the Qinghai-Tibetan Plateau (QTP), respectively. Soil water, which can be affected by permafrost thawing and precipitation, is important for vegetation growth in ... ...

Abstract	Alpine grassland and permafrost occupy about two thirds and one half of the total area of the Qinghai-Tibetan Plateau (QTP), respectively. Soil water, which can be affected by permafrost thawing and precipitation, is important for vegetation growth in this region. It is therefore vital to consider the effects of both thawing and precipitation when studying the effect of climate warming on alpine grassland on the QTP. In this study, we examined two adjacent basins, one semiarid and the other semihumid, in the northeastern section of the QTP. We used remote sensing data to compare fractional vegetation cover (FVC) and the relationships between FVC and land surface temperature (LST) in different types of frozen ground; the samples were analogous to a chronosequence of climate warming and permafrost thawing. Our analysis produced three significant results: (1) the FVCs of the semihumid basin were significantly greater than those of the semiarid basin for most types of frozen ground (p < 0.05); (2) the changes in FVC along the climate warming and permafrost thawing chronosequence were different in the two basins, with the maximum FVC occurring on the transition permafrost zone in the semiarid basin and on the seasonal frost zone in the semihumid basin; and (3) at the peak of the growing season, only the three warmest types of frozen ground in the semiarid basin had a negative relationship between FVC and LST, suggesting that vegetation growth was limited by water. Therefore, we concluded that the responses of alpine grassland to climate warming in the permafrost regions are complicated by precipitation and permafrost thawing; specifically, grasslands will not necessarily simply degrade as the climate warms, as suggested by previous plot-scale studies.
Schlagwörter	basins ; chronosequences ; fractional vegetation cover ; frost ; global warming ; grasslands ; growing season ; permafrost ; soil water ; spatial data ; surface temperature ; thawing ; China
Sprache	Englisch
Erscheinungsverlauf	2015-02
Umfang	p. 125-131.
Erscheinungsort	Institute of Arctic and Alpine Research (INSTAAR), University of Colorado
Dokumenttyp	Artikel
ZDB-ID	2045941-5
ISSN	1938-4246 ; 1523-0430
ISSN (online)	1938-4246
ISSN	1523-0430
DOI	10.1657%2FAAAR0013-098
Datenquelle	NAL Katalog (AGRICOLA)

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Artikel: Spatial and temporal variations of albedo on nine glaciers in western China from 2000 to 2011

Wang, Jie / Ye, Baisheng / Cui, Yuhuan / He, Xiaobo / Yang, Guojing

Hydrological processes. 2014 Apr. 30, v. 28, no. 9

2014

Abstract: This research demonstrates the spatiotemporal variations of albedo on nine glaciers in western China during 2000–2011, by the albedo derived from two types of datasets: Landsat TM/ETM + images and MOD10A1 product. Then, the influence factors of glacier ... ...

Abstract	This research demonstrates the spatiotemporal variations of albedo on nine glaciers in western China during 2000–2011, by the albedo derived from two types of datasets: Landsat TM/ETM + images and MOD10A1 product. Then, the influence factors of glacier albedo and its relationship with glacier mass balance are also analyzed by the correlation approach, which is frequently used in geostatistics. The paper finds that there are different spatiotemporal variations over the glaciers in western China: (1) For a single glacier, the albedo varies gently with altitude on its tongue and increases fast in the middle part, while in the accumulation zones, the albedo value appears in the form of fluctuation. This could provide a quantitative method to retrieve the snowline by determining the threshold albedo value of snowpack and bare ice. (2) For the glaciers in western China, the albedo decreases with distance to the center of Tibetan Plateau (TP). This may relate to the elevation of glacier, for the speed of glacier retreat highly depends on air temperature. (3) In the summer period, albedo on most glaciers declines over the last 12 years, and it decreases much faster in southeastern TP than other regions, for which air temperature overwhelms the black carbon concentration. In addition, the trend of glacier albedo in summer is greatly correlated with that of measured glacier mass balance, which implies that the long‐term albedo datasets by remote sensing technology could be used to monitor and predict the change of glacier mass balance in the future. Copyright © 2013 John Wiley & Sons, Ltd.
Schlagwörter	Landsat ; air temperature ; altitude ; carbon ; data collection ; glaciers ; ice ; remote sensing ; snowpack ; summer ; China
Sprache	Englisch
Erscheinungsverlauf	2014-0430
Umfang	p. 3454-3465.
Dokumenttyp	Artikel
ZDB-ID	1479953-4
ISSN	1099-1085 ; 0885-6087
ISSN (online)	1099-1085
ISSN	0885-6087
DOI	10.1002/hyp.9883
Datenquelle	NAL Katalog (AGRICOLA)

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Artikel: Inconsistencies of precipitation in the eastern and central Tibetan Plateau between surface adjusted data and reanalysis

You, Qinglong / Fraedrich, Klaus / Ren, Guoyu / Ye, Baisheng / Meng, Xianhong / Kang, Shichang

Theoretical and applied climatology. 2012 Aug., v. 109, no. 3-4

2012

Abstract: The Tibetan Plateau (TP) is the source of many Asian river systems and serves as “the Asian water tower”. Precipitation variability is a strong component of both hydrological processes and energy cycles, and the study of precipitation in the TP is of ... ...

Abstract	The Tibetan Plateau (TP) is the source of many Asian river systems and serves as “the Asian water tower”. Precipitation variability is a strong component of both hydrological processes and energy cycles, and the study of precipitation in the TP is of great importance in the content of global warming. In this study, the annual and seasonal (spring: MAM; summer: JJA; autumn: SON; and winter: DJF) variations in precipitation are investigated in the eastern and central TP during 1961–2007, based on surface raw and adjusted observations as well as both NCEP/NCAR (1961–2007) and ERA-40 (1961–2001) reanalyses. The adjusted precipitation in the TP is higher than raw values on both the annual and seasonal basis due to adjustments of solid precipitation by a bias experiential model. At the annual spring and winter scales, the adjusted precipitation shows a significant increase calculated by the Mann–Kendall trend test. Compared with adjusted precipitation; both NCEP/NCAR and ERA-40 reanalyses capture the broad spatial distributions of mean annual and seasonal precipitation, but are less good at repeating the decadal variability. Both reanalyses show the drying phenomena in most regions and fail to represent the change patterns of precipitation observed by the adjusted observations. Both NCEP/NCAR and ERA-40 have larger inconsistencies which may be caused by the differences between actual and model topography. This suggests that it is crucial to use the adjusted precipitation in the climate research and reanalysis products should be paid more attention in the TP.
Schlagwörter	atmospheric precipitation ; autumn ; climate ; global warming ; models ; plateaus ; rivers ; spring ; summer ; topography ; winter
Sprache	Englisch
Erscheinungsverlauf	2012-08
Umfang	p. 485-496.
Erscheinungsort	Springer-Verlag
Dokumenttyp	Artikel
ZDB-ID	1463177-5
ISSN	1434-4483 ; 0177-798X
ISSN (online)	1434-4483
ISSN	0177-798X
DOI	10.1007/s00704-012-0594-1
Datenquelle	NAL Katalog (AGRICOLA)

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Artikel: Stable isotopes in precipitation in Xilin River Basin, northern China and their implications

Wu, Jinkui / Ding, Yongjian / Ye, Baisheng / Yang, Qiyue / Hou, Dianjiong / Xue, Liyang

Chinese geographical science. 2012 Oct., v. 22, no. 5

2012

Abstract: Under the increasing pressure of water shortage and steppe degradation, information on the hydrological cycle in steppe region in Inner Mongolia, China is urgently needed. An intensive investigation of the temporal variations of δD and δ18O in ... ...

Abstract	Under the increasing pressure of water shortage and steppe degradation, information on the hydrological cycle in steppe region in Inner Mongolia, China is urgently needed. An intensive investigation of the temporal variations of δD and δ18O in precipitation was conducted in 2007–2008 in the Xilin River Basin, Inner Mongolia in the northern China. The δD and δ18O values for 54 precipitation samples range from +1.1‰ to −34.7‰ and −3.0‰ to −269‰, respectively. This wide range indicates that stable isotopes in precipitation are primarily controlled by different condensation mechanisms as a function of air temperature and varying sources of vapor. The relationship between δD and δ18O defined a well constrained line given by δD = 7.89 δ 18 O + 9.5, which is nearly identical to the Meteoric Water Line in the northern China. The temperature effect is clearly displayed in this area. The results of backward trajectory of each precipitation day show that the vapor of the precipitation in cold season (October to March) mainly originates from the west while the moisture source is more complicated in warm season (April to September). A light precipitation amount effect existes at the precipitation event scale in this area. The vapor source of precipitation with higher d-excesses are mainly from the west wind or neighboring inland area and precipitation with lower d-excesses from a monsoon source from the southeastern China.
Schlagwörter	air temperature ; cold season ; condensation ; hydrologic cycle ; monsoon season ; stable isotopes ; steppes ; temporal variation ; vapors ; warm season ; water shortages ; watersheds ; wind direction ; China
Sprache	Englisch
Erscheinungsverlauf	2012-10
Umfang	p. 531-540.
Erscheinungsort	Springer-Verlag
Dokumenttyp	Artikel
ZDB-ID	2268241-7
ISSN	1993-064X ; 1002-0063
ISSN (online)	1993-064X
ISSN	1002-0063
DOI	10.1007/s11769-012-0543-z
Datenquelle	NAL Katalog (AGRICOLA)

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