BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
C-118, C-117, C-116, C-115, C-114, C-113, C-112, C-111, C-110, C-109, C-108, C-107, C-106, C-105, C-104, C-103, C-102, C-101, C-100, C-99, C-98, C-97, C-96, C-95, C-94, C-93, C-92, C-91, C-90, C-89, C-88, C-87, C-86, C-85, C-84, C-83, C-82, C-81, C-80, C-79, C-78, C-77, C-76, C-75, C-74, C-73, C-72, C-71, C-70, C-69, C-68, C-67, C-66, C-65, C-64, C-63, C-62, C-61, C-60, C-59, C-58, C-57, C-56, C-55, C-54, C-53, C-52, C-51, C-50, C-49, C-48, C-47, C-46, C-45, C-44, C-43, C-42, C-41, C-40, C-39, C-38, C-37, C-36, C-35, C-33, C-32, C-31, C-30, C-29, C-28, C-27, C-26, C-25, C-24, C-23, C-22, C-21, C-20, C-19, C-18, C-17, C-16, C-15, C-14, C-13, C-12, C-11, C-10, C-9, C-8, C-7, C-6, C-5, C-4, C-3, C-2, C-1
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D - Physics of the Atmosphere
D-79, D-78, D-77, D-76, D-75, D-74, D-73, D-72, D-71, D-70, D-69, D-68, D-67, D-66, D-65, D-64, D-63, D-62, D-61, D-60, D-59, D-58, D-57, D-56, D-55, D-54, D-53, D-52, D-51, D-50, D-49, D-48, D-47, D-46, D-44, D-45, D-43, D-42, D-41, D-40, D-39, D-38, D-37, D-35, D-34, D-33, D-32, D-31, D-30, D-28, D-27, D-26, D-25, D-24, D-23, D-22, D-21, D-20, D-19, D-18, D-17, D-16, D-15, D-14, D-13, D-12, D-11, D-10, D-9, D-8, D-7, D-6, D-5, D-4, D-3, D-2, D-1
- E - Hydrology
- P - Polar Research
- M - Miscellanea
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Browse - Volume list
Results of Atmospheric Electricity and Meteorological Observations. S. Kalinowski Geophysical Observatory at Świder - 1996
Author(s):
Volume: 299
Series: D-49
Volume: 299
Series: D-49
The present issue contains the results of recordings of some elements of atmospheric electricity and daily observations of major meteorological factors noted at the S. Kalinowski Geophysical Observatory of the Polish Academy of Sciences at Świder in 1996.
Results of Geomagnetic Observations, Hel Geophysical Observatory 1996
Author(s): Czyszek A., Czyszek J.
Volume: 297
Series: C-62
Volume: 297
Series: C-62
This volume contains the results of observations of the Earth magnetic field for the year 1996, carried out at the Geophysical Observatory at Hel near Gdańsk. It is a consecutive 19-th report of similar results published since 1966.
Results of Geomagnetic Observations, Belsk 1996
Author(s): Reda J.
Volume: 296
Series: C-61
Volume: 296
Series: C-61
The publication contains results of geomagnetic observations performed in 1996; it is a consecutive, 31-st issue in the series of yearbooks listing observations of the natural magnetic field of the Earth at the Central Geophysical Observatory at Belsk.
Impact of Climate Change on Water Resources in Poland
Author(s): Kaczmarek Z., Napiórkowski J., Jurak D.
Volume: 295
Series: E-1
Volume: 295
Series: E-1
With 1,500 m3 of annual availability of per capita water supply, unevenly distributed in time and space, Poland is scarce in water in a large part of the country. A comparison of water availability in Poland and some European countries is shown in Fig. 1. Variations of country's runoff range between 34.4 km3 in 1952 and 79.5 km3 in 1981 (Fig. 2). Due to interannual and intra-annual variability (Fig. 3) of hydrologic processes, the reliable water resources, available by 95% of time, are equal to about 22 km3. Due to environmental constraints only 30% to 40% of these resources may be effectively used be agriculture, industry, or population for residential needs. Despite of natural water scarcity and some improvements in last years, Poland's economy is still water intensive. For example, the efficiency of water use in industry is, at present, three to four times lower in Poland than in most of West European countries.
Podstawowe Problemy Głębokich Badań Geofizycznych i Geologicznych Obszaru Polski *** Basic Problems of Deep Geophysical and Geological Investigations of Poland
Author(s): Guterch A., Lewandowski M., Dadlez R., Grad M., Kutek J., Żelaźniewicz A.
Volume: 294
Series: M-20
Volume: 294
Series: M-20
Głębokie badania geologiczne, prowadzone w różnych częściach naszego globu, wykazały ponad wszelką wątpliwość, że ewolucja geologiczna kompleksu osadowego skorupy ziemskiej - bardzo istotnego z punktu widzenia geologii poszukiwawczej - pozostaje w ścisłym związku z budową i ewolucją jego starszego podłoża.