Measuring evapotranspiration by hydrological methods (Record no. 51433)
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| 000 -LEADER | |
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| fixed length control field | 01883nam a2200181Ia 4500 |
| 003 - CONTROL NUMBER IDENTIFIER | |
| control field | MX-MdCICY |
| 005 - DATE AND TIME OF LATEST TRANSACTION | |
| control field | 20250625160207.0 |
| 040 ## - CATALOGING SOURCE | |
| Transcribing agency | CICY |
| 090 ## - LOCALLY ASSIGNED LC-TYPE CALL NUMBER (OCLC); LOCAL CALL NUMBER (RLIN) | |
| Classification number (OCLC) (R) ; Classification number, CALL (RLIN) (NR) | B-17270 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
| fixed length control field | 250602s9999 xx |||||s2 |||| ||und|d |
| 245 10 - TITLE STATEMENT | |
| Title | Measuring evapotranspiration by hydrological methods |
| 490 0# - SERIES STATEMENT | |
| Volume/sequential designation | Developments in Agricultural and Managed Forest Ecology, 13, p.29-40, 1984 |
| 520 3# - SUMMARY, ETC. | |
| Summary, etc. | The measurement of evapotranspiration using the methods of micrometeorology requires a sophisticated application of advanced technology. The simpler alternatives, though they are not always less costly, are discussed, namely (1)precipitation-minus-stream discharge, (2)estimates of the changes of the water storages, either in the water table aquifer or in the unsaturated zone of the soil, (3)lysimeters, and (4)material balance methods. The accuracies attainable by these methods vary. The most precise estimate can be got from a well-designed, weighable lysimeter, but the representativeness of the exposure is always a worry for the experimenter. The least precise estimate, on a month-to-month basis, is afforded by the precipitation-minusstream discharge method, but this method can give a good estimate of annual total evapotranspiration. The range of evapotranspiration rates probably spans 0.7 mm d-1 in mid-winter, on occasions, to 5 mm d-1 in late spring if the season is a wet one. For reasonable definition of these rates on a daily basis, we are looking for a method that is accurate to ±0.2 mm d-1. Only the weighing lysimeter can achieve this. The other methods variously provide mean rates for periods of five days or longer. |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | EVAPOTRANSPIRATION |
| 700 12 - ADDED ENTRY--PERSONAL NAME | |
| Personal name | Holmes, J. W. |
| 856 40 - ELECTRONIC LOCATION AND ACCESS | |
| Uniform Resource Identifier | <a href="https://drive.google.com/file/d/1p63VDAlnmWojO8cK6OSKyZrwIe3HeCo3/view?usp=drivesdk">https://drive.google.com/file/d/1p63VDAlnmWojO8cK6OSKyZrwIe3HeCo3/view?usp=drivesdk</a> |
| Public note | Para ver el documento ingresa a Google con tu cuenta: @cicy.edu.mx |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Source of classification or shelving scheme | Clasificación local |
| Koha item type | Documentos solicitados |
| Lost status | Source of classification or shelving scheme | Damaged status | Not for loan | Collection | Home library | Current library | Shelving location | Date acquired | Total checkouts | Full call number | Date last seen | Price effective from | Koha item type |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Clasificación local | Ref1 | CICY | CICY | Documento préstamo interbibliotecario | 25.06.2025 | B-17270 | 25.06.2025 | 25.06.2025 | Documentos solicitados |
