On the use of cross-correlation analysis in studies of patterns of rainfall variability
(1987) In Journal of Hydrology 93(1-2). p.113-134- Abstract
Cross-correlation structures based on daily rainfall data recorded during a period of 5 years at 67 stations throughout Tunisia are used to examine spatial rainfall variability. Basic properties of the correlation-distance function such as cumulating period, exclusion versus inclusion of dry periods, and data volume are analysed. Analysis of the correlation patterns for each month shows that two periods (February-May, and September-November) are delimited by a period of great instability (December-January) and by the dry period (June-August). Three main rainfall regions can be distinguished, delimited and governed mainly by the topography and the coastal influence.
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/98ca75e1-51cd-4b75-aa90-b0ee919c0ad1
- author
- Berndtsson, Ronny
LU
- organization
- publishing date
- 1987-08-15
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Journal of Hydrology
- volume
- 93
- issue
- 1-2
- pages
- 113 - 134
- publisher
- Elsevier
- external identifiers
-
- scopus:0023400615
- scopus:0023518031
- ISSN
- 0022-1694
- DOI
- 10.1016/0022-1694(87)90198-3
- language
- English
- LU publication?
- yes
- id
- 98ca75e1-51cd-4b75-aa90-b0ee919c0ad1
- date added to LUP
- 2022-11-11 14:20:06
- date last changed
- 2025-10-14 11:54:45
@article{98ca75e1-51cd-4b75-aa90-b0ee919c0ad1,
abstract = {{<p>Cross-correlation structures based on daily rainfall data recorded during a period of 5 years at 67 stations throughout Tunisia are used to examine spatial rainfall variability. Basic properties of the correlation-distance function such as cumulating period, exclusion versus inclusion of dry periods, and data volume are analysed. Analysis of the correlation patterns for each month shows that two periods (February-May, and September-November) are delimited by a period of great instability (December-January) and by the dry period (June-August). Three main rainfall regions can be distinguished, delimited and governed mainly by the topography and the coastal influence.</p>}},
author = {{Berndtsson, Ronny}},
issn = {{0022-1694}},
language = {{eng}},
month = {{08}},
number = {{1-2}},
pages = {{113--134}},
publisher = {{Elsevier}},
series = {{Journal of Hydrology}},
title = {{On the use of cross-correlation analysis in studies of patterns of rainfall variability}},
url = {{http://dx.doi.org/10.1016/0022-1694(87)90198-3}},
doi = {{10.1016/0022-1694(87)90198-3}},
volume = {{93}},
year = {{1987}},
}