Balázs Székely
Biographic Data
| ID | 6527343 |
|---|---|
| NAME | Balázs Székely |
| GIVEN NAMES | Balázs |
| FAMILY NAME | Székely |
| SIGNATURE | SZÉKELY B |
| AFFILIATIONS | TU Wien |
| ORCID | 0000-0002-6552-4329 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2015 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 0 |
Palmer-type soil modelling for evapotranspiration in different climatic regions of Kenya
Reference evapotranspiration (ET0) and real evapotranspiration (ET) are vital components in hydrological processes and climate-related studies. Understanding their variability in estimation is equally crucial for micro-meteorology and agricultural planning processes. The primary goal of this study was to analyze and compare estimates of (ET0) and (ET) from two different climatic regions of Kenya using long-term quality controlled synoptic station…
Archaeological Evidence for Modern Coastal Uplift at Diu, Saurashtra Peninsula, India
There is a tank hewn into coastal Pleistocene limestone near Diu city on the Saurashtra Peninsula of western India. Site survey and a review of similar structures worldwide provide evidence that this tank could have been used for holding fish or Murex snails. The approximately 5 × 5 m tank is connected to the sea by a 1‐m‐deep canal; today it would be impossible to use the tank, given that not even the high spring tides can fill it. It is suggest…
DEM-derived markers of drainage network changes in the Eastern Alpine Foothills
The study area is situated between the uplifting Alps and the subsiding Little Hungarian Plain, between 16°–17° E and 47°–47.5° N. The differential vertical motion implies neotectonic activity and some associated geomorphologic features (e.g. wind gaps, small streams in large valleys, etc.) may be observed as a result of drainage reorganization. After ∼8.7 Ma the area was characterized by a wide alluvial plain and a marsh zone. Later on, rivers s…
No prominent works on this page.
DEM-derived markers of drainage network changes in the Eastern Alpine Foothills
The study area is situated between the uplifting Alps and the subsiding Little Hungarian Plain, between 16°–17° E and 47°–47.5° N. The differential vertical motion implies neotectonic activity and some associated geomorphologic features (e.g. wind gaps, small streams in large valleys, etc.) may be observed as a result of drainage reorganization. After ∼8.7 Ma the area was characterized by a wide alluvial plain and a marsh zone. Later on, rivers s…
Archaeological Evidence for Modern Coastal Uplift at Diu, Saurashtra Peninsula, India
There is a tank hewn into coastal Pleistocene limestone near Diu city on the Saurashtra Peninsula of western India. Site survey and a review of similar structures worldwide provide evidence that this tank could have been used for holding fish or Murex snails. The approximately 5 × 5 m tank is connected to the sea by a 1‐m‐deep canal; today it would be impossible to use the tank, given that not even the high spring tides can fill it. It is suggest…
Palmer-type soil modelling for evapotranspiration in different climatic regions of Kenya
Reference evapotranspiration (ET0) and real evapotranspiration (ET) are vital components in hydrological processes and climate-related studies. Understanding their variability in estimation is equally crucial for micro-meteorology and agricultural planning processes. The primary goal of this study was to analyze and compare estimates of (ET0) and (ET) from two different climatic regions of Kenya using long-term quality controlled synoptic station…
Geography (3 works) · Geology (3 works) · Alluvial fan (1 work) · Alluvial plain (1 work) · Alluvium (1 work) · Archaeology (1 work) · Archaeology and Historical Studies (1 work) · Atmospheric sciences (1 work) · Cartography (1 work) · Climate change (1 work)