Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin
Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Huang, Jin [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2012 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© Springer-Verlag 2012 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Stochastic environmental research and risk assessment - Springer-Verlag, 1999, 27(2012), 2 vom: 22. Juni, Seite 337-351 |
|---|---|
| Übergeordnetes Werk: |
volume:27 ; year:2012 ; number:2 ; day:22 ; month:06 ; pages:337-351 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00477-012-0607-8 |
|---|
| Katalog-ID: |
OLC2058735862 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2058735862 | ||
| 003 | DE-627 | ||
| 005 | 20230502110111.0 | ||
| 007 | tu | ||
| 008 | 200820s2012 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s00477-012-0607-8 |2 doi | |
| 035 | |a (DE-627)OLC2058735862 | ||
| 035 | |a (DE-He213)s00477-012-0607-8-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 333.7 |q VZ |
| 082 | 0 | 4 | |a 550 |q VZ |
| 084 | |a 43.03$jMethoden der Umweltforschung und des Umweltschutzes |2 bkl | ||
| 084 | |a 38.85$jHydrologie: Allgemeines |2 bkl | ||
| 084 | |a 58.50$jUmwelttechnik: Allgemeines |2 bkl | ||
| 084 | |a 52.23$jFluidtechnik |2 bkl | ||
| 100 | 1 | |a Huang, Jin |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin |
| 264 | 1 | |c 2012 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Springer-Verlag 2012 | ||
| 520 | |a Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. | ||
| 650 | 4 | |a Rainfall erosivity | |
| 650 | 4 | |a Yangtze River basin | |
| 650 | 4 | |a China | |
| 650 | 4 | |a Trends | |
| 650 | 4 | |a Changes | |
| 700 | 1 | |a Zhang, Jinchi |4 aut | |
| 700 | 1 | |a Zhang, Zengxin |4 aut | |
| 700 | 1 | |a Xu, Chong-Yu |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Stochastic environmental research and risk assessment |d Springer-Verlag, 1999 |g 27(2012), 2 vom: 22. Juni, Seite 337-351 |w (DE-627)269538283 |w (DE-600)1475430-7 |w (DE-576)077885473 |x 1436-3240 |7 nnns |
| 773 | 1 | 8 | |g volume:27 |g year:2012 |g number:2 |g day:22 |g month:06 |g pages:337-351 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/s00477-012-0607-8 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_267 | ||
| 912 | |a GBV_ILN_2006 | ||
| 912 | |a GBV_ILN_2018 | ||
| 912 | |a GBV_ILN_4277 | ||
| 936 | b | k | |a 43.03$jMethoden der Umweltforschung und des Umweltschutzes |q VZ |0 106416952 |0 (DE-625)106416952 |
| 936 | b | k | |a 38.85$jHydrologie: Allgemeines |q VZ |0 106421905 |0 (DE-625)106421905 |
| 936 | b | k | |a 58.50$jUmwelttechnik: Allgemeines |q VZ |0 10641707X |0 (DE-625)10641707X |
| 936 | b | k | |a 52.23$jFluidtechnik |q VZ |0 106419870 |0 (DE-625)106419870 |
| 951 | |a AR | ||
| 952 | |d 27 |j 2012 |e 2 |b 22 |c 06 |h 337-351 | ||
| author_variant |
j h jh j z jz z z zz c y x cyx |
|---|---|
| matchkey_str |
article:14363240:2012----::ptaadeprlaitosnanalrsvtdrn1620 |
| hierarchy_sort_str |
2012 |
| bklnumber |
43.03$jMethoden der Umweltforschung und des Umweltschutzes 38.85$jHydrologie: Allgemeines 58.50$jUmwelttechnik: Allgemeines 52.23$jFluidtechnik |
| publishDate |
2012 |
| allfields |
10.1007/s00477-012-0607-8 doi (DE-627)OLC2058735862 (DE-He213)s00477-012-0607-8-p DE-627 ger DE-627 rakwb eng 333.7 VZ 550 VZ 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik bkl Huang, Jin verfasserin aut Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. Rainfall erosivity Yangtze River basin China Trends Changes Zhang, Jinchi aut Zhang, Zengxin aut Xu, Chong-Yu aut Enthalten in Stochastic environmental research and risk assessment Springer-Verlag, 1999 27(2012), 2 vom: 22. Juni, Seite 337-351 (DE-627)269538283 (DE-600)1475430-7 (DE-576)077885473 1436-3240 nnns volume:27 year:2012 number:2 day:22 month:06 pages:337-351 https://doi.org/10.1007/s00477-012-0607-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2018 GBV_ILN_4277 43.03$jMethoden der Umweltforschung und des Umweltschutzes VZ 106416952 (DE-625)106416952 38.85$jHydrologie: Allgemeines VZ 106421905 (DE-625)106421905 58.50$jUmwelttechnik: Allgemeines VZ 10641707X (DE-625)10641707X 52.23$jFluidtechnik VZ 106419870 (DE-625)106419870 AR 27 2012 2 22 06 337-351 |
| spelling |
10.1007/s00477-012-0607-8 doi (DE-627)OLC2058735862 (DE-He213)s00477-012-0607-8-p DE-627 ger DE-627 rakwb eng 333.7 VZ 550 VZ 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik bkl Huang, Jin verfasserin aut Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. Rainfall erosivity Yangtze River basin China Trends Changes Zhang, Jinchi aut Zhang, Zengxin aut Xu, Chong-Yu aut Enthalten in Stochastic environmental research and risk assessment Springer-Verlag, 1999 27(2012), 2 vom: 22. Juni, Seite 337-351 (DE-627)269538283 (DE-600)1475430-7 (DE-576)077885473 1436-3240 nnns volume:27 year:2012 number:2 day:22 month:06 pages:337-351 https://doi.org/10.1007/s00477-012-0607-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2018 GBV_ILN_4277 43.03$jMethoden der Umweltforschung und des Umweltschutzes VZ 106416952 (DE-625)106416952 38.85$jHydrologie: Allgemeines VZ 106421905 (DE-625)106421905 58.50$jUmwelttechnik: Allgemeines VZ 10641707X (DE-625)10641707X 52.23$jFluidtechnik VZ 106419870 (DE-625)106419870 AR 27 2012 2 22 06 337-351 |
| allfields_unstemmed |
10.1007/s00477-012-0607-8 doi (DE-627)OLC2058735862 (DE-He213)s00477-012-0607-8-p DE-627 ger DE-627 rakwb eng 333.7 VZ 550 VZ 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik bkl Huang, Jin verfasserin aut Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. Rainfall erosivity Yangtze River basin China Trends Changes Zhang, Jinchi aut Zhang, Zengxin aut Xu, Chong-Yu aut Enthalten in Stochastic environmental research and risk assessment Springer-Verlag, 1999 27(2012), 2 vom: 22. Juni, Seite 337-351 (DE-627)269538283 (DE-600)1475430-7 (DE-576)077885473 1436-3240 nnns volume:27 year:2012 number:2 day:22 month:06 pages:337-351 https://doi.org/10.1007/s00477-012-0607-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2018 GBV_ILN_4277 43.03$jMethoden der Umweltforschung und des Umweltschutzes VZ 106416952 (DE-625)106416952 38.85$jHydrologie: Allgemeines VZ 106421905 (DE-625)106421905 58.50$jUmwelttechnik: Allgemeines VZ 10641707X (DE-625)10641707X 52.23$jFluidtechnik VZ 106419870 (DE-625)106419870 AR 27 2012 2 22 06 337-351 |
| allfieldsGer |
10.1007/s00477-012-0607-8 doi (DE-627)OLC2058735862 (DE-He213)s00477-012-0607-8-p DE-627 ger DE-627 rakwb eng 333.7 VZ 550 VZ 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik bkl Huang, Jin verfasserin aut Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. Rainfall erosivity Yangtze River basin China Trends Changes Zhang, Jinchi aut Zhang, Zengxin aut Xu, Chong-Yu aut Enthalten in Stochastic environmental research and risk assessment Springer-Verlag, 1999 27(2012), 2 vom: 22. Juni, Seite 337-351 (DE-627)269538283 (DE-600)1475430-7 (DE-576)077885473 1436-3240 nnns volume:27 year:2012 number:2 day:22 month:06 pages:337-351 https://doi.org/10.1007/s00477-012-0607-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2018 GBV_ILN_4277 43.03$jMethoden der Umweltforschung und des Umweltschutzes VZ 106416952 (DE-625)106416952 38.85$jHydrologie: Allgemeines VZ 106421905 (DE-625)106421905 58.50$jUmwelttechnik: Allgemeines VZ 10641707X (DE-625)10641707X 52.23$jFluidtechnik VZ 106419870 (DE-625)106419870 AR 27 2012 2 22 06 337-351 |
| allfieldsSound |
10.1007/s00477-012-0607-8 doi (DE-627)OLC2058735862 (DE-He213)s00477-012-0607-8-p DE-627 ger DE-627 rakwb eng 333.7 VZ 550 VZ 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik bkl Huang, Jin verfasserin aut Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. Rainfall erosivity Yangtze River basin China Trends Changes Zhang, Jinchi aut Zhang, Zengxin aut Xu, Chong-Yu aut Enthalten in Stochastic environmental research and risk assessment Springer-Verlag, 1999 27(2012), 2 vom: 22. Juni, Seite 337-351 (DE-627)269538283 (DE-600)1475430-7 (DE-576)077885473 1436-3240 nnns volume:27 year:2012 number:2 day:22 month:06 pages:337-351 https://doi.org/10.1007/s00477-012-0607-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2018 GBV_ILN_4277 43.03$jMethoden der Umweltforschung und des Umweltschutzes VZ 106416952 (DE-625)106416952 38.85$jHydrologie: Allgemeines VZ 106421905 (DE-625)106421905 58.50$jUmwelttechnik: Allgemeines VZ 10641707X (DE-625)10641707X 52.23$jFluidtechnik VZ 106419870 (DE-625)106419870 AR 27 2012 2 22 06 337-351 |
| language |
English |
| source |
Enthalten in Stochastic environmental research and risk assessment 27(2012), 2 vom: 22. Juni, Seite 337-351 volume:27 year:2012 number:2 day:22 month:06 pages:337-351 |
| sourceStr |
Enthalten in Stochastic environmental research and risk assessment 27(2012), 2 vom: 22. Juni, Seite 337-351 volume:27 year:2012 number:2 day:22 month:06 pages:337-351 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Rainfall erosivity Yangtze River basin China Trends Changes |
| dewey-raw |
333.7 |
| isfreeaccess_bool |
false |
| container_title |
Stochastic environmental research and risk assessment |
| authorswithroles_txt_mv |
Huang, Jin @@aut@@ Zhang, Jinchi @@aut@@ Zhang, Zengxin @@aut@@ Xu, Chong-Yu @@aut@@ |
| publishDateDaySort_date |
2012-06-22T00:00:00Z |
| hierarchy_top_id |
269538283 |
| dewey-sort |
3333.7 |
| id |
OLC2058735862 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2058735862</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502110111.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2012 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00477-012-0607-8</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2058735862</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00477-012-0607-8-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">333.7</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.03$jMethoden der Umweltforschung und des Umweltschutzes</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.85$jHydrologie: Allgemeines</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">58.50$jUmwelttechnik: Allgemeines</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">52.23$jFluidtechnik</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Huang, Jin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 2012</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Rainfall erosivity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Yangtze River basin</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">China</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Trends</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Changes</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Jinchi</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Zengxin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Chong-Yu</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Stochastic environmental research and risk assessment</subfield><subfield code="d">Springer-Verlag, 1999</subfield><subfield code="g">27(2012), 2 vom: 22. Juni, Seite 337-351</subfield><subfield code="w">(DE-627)269538283</subfield><subfield code="w">(DE-600)1475430-7</subfield><subfield code="w">(DE-576)077885473</subfield><subfield code="x">1436-3240</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:27</subfield><subfield code="g">year:2012</subfield><subfield code="g">number:2</subfield><subfield code="g">day:22</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:337-351</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00477-012-0607-8</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">43.03$jMethoden der Umweltforschung und des Umweltschutzes</subfield><subfield code="q">VZ</subfield><subfield code="0">106416952</subfield><subfield code="0">(DE-625)106416952</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.85$jHydrologie: Allgemeines</subfield><subfield code="q">VZ</subfield><subfield code="0">106421905</subfield><subfield code="0">(DE-625)106421905</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">58.50$jUmwelttechnik: Allgemeines</subfield><subfield code="q">VZ</subfield><subfield code="0">10641707X</subfield><subfield code="0">(DE-625)10641707X</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">52.23$jFluidtechnik</subfield><subfield code="q">VZ</subfield><subfield code="0">106419870</subfield><subfield code="0">(DE-625)106419870</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">27</subfield><subfield code="j">2012</subfield><subfield code="e">2</subfield><subfield code="b">22</subfield><subfield code="c">06</subfield><subfield code="h">337-351</subfield></datafield></record></collection>
|
| author |
Huang, Jin |
| spellingShingle |
Huang, Jin ddc 333.7 ddc 550 bkl 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik misc Rainfall erosivity misc Yangtze River basin misc China misc Trends misc Changes Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin |
| authorStr |
Huang, Jin |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)269538283 |
| format |
Article |
| dewey-ones |
333 - Economics of land & energy 550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
1436-3240 |
| topic_title |
333.7 VZ 550 VZ 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik bkl Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin Rainfall erosivity Yangtze River basin China Trends Changes |
| topic |
ddc 333.7 ddc 550 bkl 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik misc Rainfall erosivity misc Yangtze River basin misc China misc Trends misc Changes |
| topic_unstemmed |
ddc 333.7 ddc 550 bkl 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik misc Rainfall erosivity misc Yangtze River basin misc China misc Trends misc Changes |
| topic_browse |
ddc 333.7 ddc 550 bkl 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik misc Rainfall erosivity misc Yangtze River basin misc China misc Trends misc Changes |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Stochastic environmental research and risk assessment |
| hierarchy_parent_id |
269538283 |
| dewey-tens |
330 - Economics 550 - Earth sciences & geology |
| hierarchy_top_title |
Stochastic environmental research and risk assessment |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)269538283 (DE-600)1475430-7 (DE-576)077885473 |
| title |
Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin |
| ctrlnum |
(DE-627)OLC2058735862 (DE-He213)s00477-012-0607-8-p |
| title_full |
Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin |
| author_sort |
Huang, Jin |
| journal |
Stochastic environmental research and risk assessment |
| journalStr |
Stochastic environmental research and risk assessment |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
300 - Social sciences 500 - Science |
| recordtype |
marc |
| publishDateSort |
2012 |
| contenttype_str_mv |
txt |
| container_start_page |
337 |
| author_browse |
Huang, Jin Zhang, Jinchi Zhang, Zengxin Xu, Chong-Yu |
| container_volume |
27 |
| class |
333.7 VZ 550 VZ 43.03$jMethoden der Umweltforschung und des Umweltschutzes bkl 38.85$jHydrologie: Allgemeines bkl 58.50$jUmwelttechnik: Allgemeines bkl 52.23$jFluidtechnik bkl |
| format_se |
Aufsätze |
| author-letter |
Huang, Jin |
| doi_str_mv |
10.1007/s00477-012-0607-8 |
| normlink |
106416952 106421905 10641707X 106419870 |
| normlink_prefix_str_mv |
106416952 (DE-625)106416952 106421905 (DE-625)106421905 10641707X (DE-625)10641707X 106419870 (DE-625)106419870 |
| dewey-full |
333.7 550 |
| title_sort |
spatial and temporal variations in rainfall erosivity during 1960–2005 in the yangtze river basin |
| title_auth |
Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin |
| abstract |
Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. © Springer-Verlag 2012 |
| abstractGer |
Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. © Springer-Verlag 2012 |
| abstract_unstemmed |
Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years. © Springer-Verlag 2012 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2018 GBV_ILN_4277 |
| container_issue |
2 |
| title_short |
Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin |
| url |
https://doi.org/10.1007/s00477-012-0607-8 |
| remote_bool |
false |
| author2 |
Zhang, Jinchi Zhang, Zengxin Xu, Chong-Yu |
| author2Str |
Zhang, Jinchi Zhang, Zengxin Xu, Chong-Yu |
| ppnlink |
269538283 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s00477-012-0607-8 |
| up_date |
2024-07-03T20:00:31.238Z |
| _version_ |
1803589340353265664 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2058735862</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502110111.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2012 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00477-012-0607-8</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2058735862</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00477-012-0607-8-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">333.7</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.03$jMethoden der Umweltforschung und des Umweltschutzes</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.85$jHydrologie: Allgemeines</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">58.50$jUmwelttechnik: Allgemeines</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">52.23$jFluidtechnik</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Huang, Jin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spatial and temporal variations in rainfall erosivity during 1960–2005 in the Yangtze River basin</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 2012</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Water resources and soil erosion are the most important environmental concerns in the Yangtze River basin, where soil erosion and sediment yield are closely related to rainfall erosivity. The present study explores the spatial and temporal changing patterns of the rainfall erosivity in the Yangtze River basin of China during 1960–2005 at annual, seasonal and monthly scales. The Mann–Kendall test is employed to detect the trends during 1960–2005, and the T test is applied to investigate possible changes between 1991–2005 and 1960–1990. Meanwhile the Rescaled Range Analysis is used for exploring future trend of rainfall erosivity. Moreover the continuous wavelet transform technique is using studying the periodicity of the rainfall erosivity. The results show that: (1) The Yangtze River basin is an area characterized by uneven spatial distribution of rainfall erosivity in China, with the annual average rainfall erosivity range from 131.21 to 16842 MJ mm $ ha^{−1} $ $ h^{−1} $. (2) Although the directions of trends in annual rainfall erosivity at most stations are upward, only 22 stations have significant trends at the 90 % confidence level, and these stations are mainly located in the Jinshajiang River basin and Boyang Lake basin. Winter and summer are the seasons showing strong upward trends. For the monthly series, significant increasing trends are mainly found during January, June and July. (3) Generally speaking, the results detected by the T test are quite consistent with those detected by the Mann–Kendall test. (4) The rainfall erosivity of Yangtze River basin during winter and summer will maintain a detected significant increasing trend in the near future, which may bring greater risks to soil erosion. (5) The annual and seasonal erosivity of Yangtze River basin all have one significant periodicity of 2–4 years.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Rainfall erosivity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Yangtze River basin</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">China</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Trends</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Changes</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Jinchi</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Zengxin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Chong-Yu</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Stochastic environmental research and risk assessment</subfield><subfield code="d">Springer-Verlag, 1999</subfield><subfield code="g">27(2012), 2 vom: 22. Juni, Seite 337-351</subfield><subfield code="w">(DE-627)269538283</subfield><subfield code="w">(DE-600)1475430-7</subfield><subfield code="w">(DE-576)077885473</subfield><subfield code="x">1436-3240</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:27</subfield><subfield code="g">year:2012</subfield><subfield code="g">number:2</subfield><subfield code="g">day:22</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:337-351</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00477-012-0607-8</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">43.03$jMethoden der Umweltforschung und des Umweltschutzes</subfield><subfield code="q">VZ</subfield><subfield code="0">106416952</subfield><subfield code="0">(DE-625)106416952</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.85$jHydrologie: Allgemeines</subfield><subfield code="q">VZ</subfield><subfield code="0">106421905</subfield><subfield code="0">(DE-625)106421905</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">58.50$jUmwelttechnik: Allgemeines</subfield><subfield code="q">VZ</subfield><subfield code="0">10641707X</subfield><subfield code="0">(DE-625)10641707X</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">52.23$jFluidtechnik</subfield><subfield code="q">VZ</subfield><subfield code="0">106419870</subfield><subfield code="0">(DE-625)106419870</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">27</subfield><subfield code="j">2012</subfield><subfield code="e">2</subfield><subfield code="b">22</subfield><subfield code="c">06</subfield><subfield code="h">337-351</subfield></datafield></record></collection>
|
| score |
7.3996277 |