Verifikacija modela evapotranspiracije: hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave
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| Main Author: | |
|---|---|
| Format: | Book |
| Published: |
Beograd
Geografski Inst. Jovan Cvijić Srpske Akad. Nauka i Umetnosti
2010
|
| Series: | Posebna izdanja / Geografski Institut Jovan Cvijić
78 |
| Subjects: | |
| Online Access: | Abstract Inhaltsverzeichnis |
| Item Description: | PST: Verification of the evapotranspiration model. - In kyrill. Schr., serb. - Zsfassung in engl. Sprache |
| Physical Description: | 304 S. Ill., graph. Darst., Kt. |
| ISBN: | 9788680029498 |
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| 100 | 1 | |a Nikolić, Jugoslav |d 1955- |e Verfasser |0 (DE-588)102759848X |4 aut | |
| 245 | 1 | 0 | |a Verifikacija modela evapotranspiracije |b hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave |c Jugoslav Nikolić |
| 264 | 1 | |a Beograd |b Geografski Inst. Jovan Cvijić Srpske Akad. Nauka i Umetnosti |c 2010 | |
| 300 | |a 304 S. |b Ill., graph. Darst., Kt. | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b n |2 rdamedia | ||
| 338 | |b nc |2 rdacarrier | ||
| 490 | 1 | |a Posebna izdanja / Geografski Institut Jovan Cvijić |v 78 | |
| 500 | |a PST: Verification of the evapotranspiration model. - In kyrill. Schr., serb. - Zsfassung in engl. Sprache | ||
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| 689 | 0 | 0 | |a Zapadna Morava |0 (DE-588)4621509-8 |D g |
| 689 | 0 | 1 | |a Evapotranspiration |0 (DE-588)4219549-4 |D s |
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Record in the Search Index
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|---|---|
| adam_text | 14.
SUMMARY
The evapotranspiration is one of the most important processes of water
circulation. The evapotranspiration, along with precipitation and total runoff,
represents the basic element of the water balance, which is difficult to determine
quantitatively.
The accurate spatial determination of evapotranspiration has strategic
importance for various scientific disciplines and practical applications, especially
in waterpower engineering, agriculture, forestry, electrical industry, construction
industry and tourism. This research represents an attempt for a more realistic
perception of an evapotranspiration in heterogeneous geological conditions by
the application of numerical model with solid physical base. The above described
model represents good physically based tool for successful solving of various
problems.
The basic equation of the model was calibrated using the data obtained
through lysimeter and meteorological measurement from experimental research.
The application and verification of the model was conducted on the upper basin
of the
Zapadna
Morava
river.
Parameterization of geological influences of terrain on the water
evaporation was performed by comparative analysis of spatial evaporation
calculated by the model and the values obtained from the water balance method.
Balancing takes into account the hydrogeological approach to terrain exploration
and the analysis of the precipitation using the verified model. Hydrogeological
research includes the analysis of physical-geographic, hydrological and
climatological conditions of terrain as well as vegetative cover,
geomorphological characteristics of terrain, elements of geological structure and
hydrogeological attributes of rocks of the selected watershed area. The elements
of the water balance were obtained from series of data and measurements, lasting
several years, of precipitation and water flow on relevant locations from the
model domain.
The input values of certain physical variables at model application were
obtained by existing measurements on available locations (meteorological
stations). An output from evapotranspiration model are monthly values in terms
of quantity of the evapotranspiration in network points
lx 1
km.
The model integrates energy and dynamic effects, and the effect of plant
physiology, whereas specific influences of various foundation rocks are
204
VERIFICATION OF THE EVAPOTRANSPIRATION MODEL
HYDROGEOLOGICAL, HYDROLOGICAL, GEOGRAPHICAL AND METEOROLOGICAL RESEARCH
ON THE CASE EXAMPLE OF
ZAPADNA
MORAVA
UPPER RIVER BASIN
parametric. The
metodology
of application, among other things, includes
digital
ized
topography with spatial and time analysis of entry parameters
obtained by existing measurements. The model domain is defined in relation to
an area of the examined river basin. The model resolution with spatial step
к
=
Δχ
=
Ay
= 1
km secures precise enough calculation of the evapotranspiration
values in heterogeneous geophysical and geological conditions of natural
environment, which conditions its spatial
variability.
In natural conditions of observed hydrogeological systems, the
evapotranspiration can be significantly influenced by physical characteristics of
terrain. The model does not explicitly include specific influences of various
geological terrains. Due to the lack of lysimetric measurements, an empirical
determination of terrain influences in the
Zapadna
Morava
upper river basin was
conducted through comparative application of the water balance. The balancing
is conducted through hydrogeological approach, paying special attention to
inflows/outflows of groundwater from basin to basin. Analyzing the
evapotranspiration obtained by an application of the model and „referential
values determined by the water balance method, enables corrections of the
evapotranspiration according to the model.
Major parameters determining the evapotranspiration process are
modularly established and integrated into the model through its basic equation.
The first step connotes updating the database from the domain of the grid-based
analysis
(Nikolić
et al,
2005).
For each unit field of
1
km2 relevant information is
updated and used as a matrix in model calculations. Input data were cartometric,
or obtained by standard physical measurements of meteorological parameters at
climate stations.
Cartographic parameters are determined using geographic maps at scale
1:25,000.
For each field, lxlkm, from the model domain, coordinates of the left
lower corner, maximum, minimum and mean land altitudes, slope and
afforestation were used. The squares including river basin were divided into
hundred smaller squares,
100x1
00m in size, for a precise calculation in the
watershed border area.
On the case example of the
Zapadna
Morava
upper river basin, the
evapotranspiration calculation model was used comparatively with the water
balance method whose basic elements are precipitation, water evaporation and
runoff.
Comparative with the numerical model for study of the
areal
evapotranspiration in the
Zapadna
Morava
upper catchment area, the method of
water balance was used that accounts precipitation, evaporation and runoff.
Perennial series of values for precipitation and flow at given river sections may
be used, under certain condition, to determine with sufficient precision the
SUMMARY
205
average water evaporation from the catchment area. The condition was a good
precipitation analysis in addition to hydrogeological investigations
(Nikolić
et al,
2007)
for relative reliability of certain assumptions (e.g. exclusion of the likely
groundwater inflow/outflow from one basin to another).
For comparative analysis of the evapotranspiration by the water balance
method, a dynamic precipitation analysis was made, which included the influence
of orography and dynamics on precipitation quantities. A given value of
precipitation, obtained by numerical analysis, was added to each elementary
field. The dynamic precipitation analysis used three-dimensional non-hydrostatic
numerical model FITNAH (Flow over Irregular Terrain with Natural and
Anthropogenic Heat Sources). The model specifically solves the representation
of orography influence on meteorological parameters
(Frenzen et
al.,
1987;
Nikolić,
2002).
The amount of precipitation is calculated by the mentioned
method.
The results of evapotranspiration calculation for the
Zapadna
Morava
upper river basin prove that the applied model is a good tool for the estimation of
the evapotranspiration.
The average values of the evapotranspiration for the
Zapadna
Morava
upper river basin according to the model are larger than the average value
obtained by balancing, which is explained by geological factors of the terrain.
The evapotranspiration determined by the model for the
Zapadna
Morava
upper
river basin comes closer to referential value, obtained by the method of water
balance, when it is multiplied with the correction coefficient
0,91.
The earlier
research showed that this coefficient in natural conditions can be somewhere in
the interval from
0,3 - 1,0,
depending on the geological characteristics of the
terrain, and presence and evolution of
karst
processes on the terrain (Nikolic J.,
2002).
The research shows that, when analyzing precipitation, the
orographie
effects should be taken into consideration, which increase precipitation with
height, along with dynamic effects that condition the size of this increase, as well
as decrease of precipitation with the further increase in height, above some
critical value. It appears that the problem is not simple and that the use of
simplified relations for precipitation interpolation can lead to substantial mistakes
in the estimation. The outcome is justification for the application of stated three-
dimensional non-hydrostatic numerical model as a better tool in the precipitation
analysis in relation to classical interpolation methods.
The described numerical model for determination of the evapo¬
transpiration in heterogeneous geological conditions represents physically based
tool for successful solution of numerous practical problems in different scientific
disciplines. The primary advantage of the mentioned model is a good physical
206
VERIFICATION OF THE EVAPOTRANSPIRATION MODEL
HYDROGEOLOGICAL, HYDROLOGICAL, GEOGRAPHICAL AND METEOROLOGICAL RESEARCH
ON THE CASE EXAMPLE OF
ZAPADNA
MORAVA
UPPER RIVER BASIN
foundation and simplicity in a practical application, that is to say implementation,
along with the use of common, available data, without excessive investments.
The research has shown that, in addition to the primary meteorological
and hydrological factors, the geology and hydrogeo
logica
I conditions can
substantially modify the water balance of an area.
САДРЖАЈ
1.
УВОД
..........................................................................................................25
2.
ПОСТАВКА
ИСТРАЖИВАЊА
..............................................................29
2.1.
Предмет и
циљ монографије
............................................................29
2.2.
Методологија истраживања
..............................................................30
2.3.
Избор
сливног подручја
.............................................. ......................34
3.
ОСНОВНИ ФИЗИЧКО ГЕОГРАФСКИ УСЛОВИ
ТЕРЕНА
ИЗАБРАНОГ
ЗА
ВЕРИФИКАЦИЈУ
МОДЕЛА
.....................39
3.1.
Положај
и
квалитативне карактеристике рељефа
изучаваног
терена
изабраног
за
верификацију
модела
..................39
3.2.
Квантитативна анализа
рељефа
изучаваног
терена
.......................43
4.
ХИДРОЛОШКИ УСЛОВИ СЛИВНОГ
ИОДРУЧЈА
ИЗАБРАНОГ ЗА
ВЕРИФИКАЦИЈУ
МОДЕЛА ЕВАПОТРАНСПИРАЦШЕ
...................................................47
4.1.
СливМоравице
..................................................................................48
4.2.
Слив
Ђетиње......................................................................................
56
4.3.
Слив
Бјелице
......................................................................................59
4.4.
Слив
Каменице
....................................
4
.............................................61
4.5.
Слив Чемернице
................................................................................62
4.6.
Специфичне хидролошке појаве
у
горњем
сливу Западне Мораве
......................................................64
4.6.1.
Дајићкојезеро
........................................................................64
4.6.2.
Језеро Округлица
...................................................................65
4.7.
Напомене
о квалитету воде
горњег
слива Западне Мораве.........................................................
66
4.8.
Основне напомене о
ерозији
подлоге
изучаваног
терена..............................................................................
68
4.9.
Површина изучаваног сливног
подручја
према
нумеричкој
анализи................................................................
73
4.10.Геометријске
карактеристике
горњег
слива Западне
Мораве..........................................................
75
5.
ОСНОВНЕ КАРАКТЕРИСТИКЕ
ХИДРОЛОШКИХ
И МЕТЕОРОЛОШКИХ СТАНИЦА
ИЗУЧАВАНОГ
ТЕРЕНА............
79
5.1.
Хидролошке станице
.........................................................................79
5.1.1.
Детаљније информације
о водомерным станицама
..........79
5.2.
Метеоролошке станице
.....................................................................85
6.
ОСНОВНЕ КЛИМАТСКЕ
КАРАКТЕРИСТИКЕ
ИЗАБРАНОГ
ТЕРЕНА
.............................................................................89
6.1.
Ваздушни притисак
...........................................................................89
6.2.
Температура ваздуха
.........................................................................92
6.3.
Влажност ваздуха
..............................................................................94
6.4.
Падавине
.............................................................................................97
6.5.
Облачност и
инсолација.
...................................................................99
6.6.
Ветар
.................................................................................................102
7.
ВЕГЕТАЦИОНИ ПОКРИВАЧ ИЗУЧАВАНОГ ТЕРЕНА
...................109
8.
ГЕОМОРФОЛОШКЕ КАРАКТЕРИСТИКЕ ИЗАБРАНОГ ТЕРЕНА
119
9.
ГЕОЛОШКА
ГРАЂА
ИСТРАЖИВАНОГ
ПОДРУЧЈА
......................135
9.1.
Приказ
досадашњих истраживања
и оцена степена истражености изучаваног
терена
.......................135
9.2.
Геолошки састав
и литостратиграфске карактеристике
терена
................................136
9.2.1.
Старији
палеозоик
...............................................................137
9.2.2.
Млађи
палеозоик
..................................................................138
9.2.2.1.
Карбон
.....................................................................138
9.2.2.2.
Перм
.........................................................................139
9.2.3.
Мезозоик
...............................................................................140
9.2.3.1.
Тријас
.......................................................................140
9.2.3.2.
Jypa...........................................................................
142
9.2.3.3.
Креда
........................................................................144
9.2.4.
Кенозоик
...............................................................................149
9.2.4.1.
Неоген
......................................................................149
9.2.4.1.
Квартпар
...................................................................151
10.
ХИДРОГЕОЛОШКЕ КАРАКТЕРИСТИКЕ
ТЕРЕНА
СЛИВНОГ
ПОДРУЧЈА
ОДАБРАНОГ ЗА
ВЕРИФИКАЦИЈУ
РАЗВИЈЕНОГ
МОДЕЛА
ЕВАПОТРАНСПИРАЦИЈЕ........................
155
10.1
.Приказ
досадашњих хидрогеолошких истраживања
и оцена степена истражености
терена
...........................................155
10.2.Хидрогеолошка
својства
терена
и
типови
издани у оквиру
подручја истраживања
........................156
10.2.1.
Збијени
mun
издани
..............................................................156
10.2.2.
Пукотииски тип издани
......................................................159
10.2.3.
Карстнитип издани
...........................................................160
10.2.4.
Условно
безводни делови терена
...................................162
Ю.З.Изворишта термалне и минералне воде
........................................163
10.4.Специфичнепојаве
..........................................................................171
11.
ЕЛЕМЕНТИ
ВОДНОГ БИЛАНСА
ИЗУЧАВАНОГ СЛИВНОГ
ПОДРУЧЈА
...............................................175
1
1.1.Отицај
у
горњем
сливу Западне Мораве
.......................................175
10.1.1.
Фактори
који
утичу на
отицај
..........................................175
10.1.2.
Структура
процеса
укупног
отицаја
................................177
10.1.3.
Прорачун укупног отицаја
горњег
слива Западне
Мораве
.............................................179
11
.2.Анализа падавина
на примеру
горњег
слива Западне
Мораве
....................................182
11.2.1.
Основне статистичке
вредности падавина
добијених мерењем
у домену
модела.
..................................182
11.2.2.
Однос
измерених
и анализом
добијених
сума падавина
.................................182
11.2.3.
Упгицај надморске
висине
слива
на суму падавина
.....................................,............................185-
11.2.4.
Запажањау
вези промена режима падавина
на изучаваном сливу
.............................................................186
12.
РЕЗУЛТАТИ ПРИМЕНЕ МОДЕЛА
ЗА
ОДРЕЂИВАЊЕ ЕВАПОТРАНСПИРАЦИЈЕ
.................................191
П.І.Евапотранспирационо
поље
...........................................................192
13.
ЗАЮЪУЧАК
.............................................................................................197
14.
SUMMARY
..............................................................................................203
15.
ЛИТЕРАТУРА
.........................................................................................207
ПРИЛОЗИ
.......................................................................................................221
|
| any_adam_object | 1 |
| author | Nikolić, Jugoslav 1955- |
| author_GND | (DE-588)102759848X |
| author_facet | Nikolić, Jugoslav 1955- |
| author_role | aut |
| author_sort | Nikolić, Jugoslav 1955- |
| author_variant | j n jn |
| building | Verbundindex |
| bvnumber | BV040528529 |
| ctrlnum | (OCoLC)820385553 (DE-599)BVBBV040528529 |
| format | Book |
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| geographic | Zapadna Morava (DE-588)4621509-8 gnd |
| geographic_facet | Zapadna Morava |
| id | DE-604.BV040528529 |
| illustrated | Illustrated |
| indexdate | 2024-07-10T00:25:49Z |
| institution | BVB |
| isbn | 9788680029498 |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-025374649 |
| oclc_num | 820385553 |
| open_access_boolean | |
| owner | DE-12 |
| owner_facet | DE-12 |
| physical | 304 S. Ill., graph. Darst., Kt. |
| publishDate | 2010 |
| publishDateSearch | 2010 |
| publishDateSort | 2010 |
| publisher | Geografski Inst. Jovan Cvijić Srpske Akad. Nauka i Umetnosti |
| record_format | marc |
| series2 | Posebna izdanja / Geografski Institut Jovan Cvijić |
| spelling | Nikolić, Jugoslav 1955- Verfasser (DE-588)102759848X aut Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave Jugoslav Nikolić Beograd Geografski Inst. Jovan Cvijić Srpske Akad. Nauka i Umetnosti 2010 304 S. Ill., graph. Darst., Kt. txt rdacontent n rdamedia nc rdacarrier Posebna izdanja / Geografski Institut Jovan Cvijić 78 PST: Verification of the evapotranspiration model. - In kyrill. Schr., serb. - Zsfassung in engl. Sprache Evapotranspiration (DE-588)4219549-4 gnd rswk-swf Zapadna Morava (DE-588)4621509-8 gnd rswk-swf Zapadna Morava (DE-588)4621509-8 g Evapotranspiration (DE-588)4219549-4 s DE-604 Geografski Institut Jovan Cvijić Posebna izdanja 78 (DE-604)BV008905274 78 Digitalisierung BSB Muenchen 2 application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025374649&sequence=000003&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Abstract Digitalisierung BSB Muenchen 2 application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025374649&sequence=000004&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis |
| spellingShingle | Nikolić, Jugoslav 1955- Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave Evapotranspiration (DE-588)4219549-4 gnd |
| subject_GND | (DE-588)4219549-4 (DE-588)4621509-8 |
| title | Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave |
| title_auth | Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave |
| title_exact_search | Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave |
| title_full | Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave Jugoslav Nikolić |
| title_fullStr | Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave Jugoslav Nikolić |
| title_full_unstemmed | Verifikacija modela evapotranspiracije hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave Jugoslav Nikolić |
| title_short | Verifikacija modela evapotranspiracije |
| title_sort | verifikacija modela evapotranspiracije hidrogeoloska hidroloska geografska i meteoroloska istrazivanja na primeru gornjet sliva zapadne morave |
| title_sub | hidrogeološka, hidrološka, geografska i meteorološka istraživanja na primeru gornjet sliva Zapadne Morave |
| topic | Evapotranspiration (DE-588)4219549-4 gnd |
| topic_facet | Evapotranspiration Zapadna Morava |
| url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025374649&sequence=000003&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025374649&sequence=000004&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA |
| volume_link | (DE-604)BV008905274 |
| work_keys_str_mv | AT nikolicjugoslav verifikacijamodelaevapotranspiracijehidrogeoloskahidroloskageografskaimeteoroloskaistrazivanjanaprimerugornjetslivazapadnemorave |