Results 161 to 170 of about 13,528 (208)

Reconstructing East Antarctic Temperature and Snowfall Variability from δ15N of N2

Bouchet M, Landais A, Klüssendorf AM, Brückner L, Legrain E, Capron E, Parrenin F, Menviel L, Grisart A, Prié F, Extier T, Jacob R, Fischer H, Traeger H, Tinner P, Schmitt J, Grimmer M.   +16 more
europepmc   +1 more source

Technetium-99 determination in low-volume samples from the global environment with accelerator mass spectrometry.

Env Sci Adv
Hain K, Adler S, Faestermann T, Fifield LK, Froehlich MB, Gülce F, Koll D, Korschinek G, Martschini M, Quinto F, Pavetich S, Pitters J, Rugel G, Tims S, Welch J, Wiederin A, Yamada M.   +16 more
europepmc   +1 more source

Spatial modeling of extreme snow depth and snow water equivalent

, 2017
openaire   +1 more source

Modelling snow water equivalent based on daily snow depths

, 2014
openaire   +1 more source

Analysis of GPR Data for Snow Water Equivalent

70th EAGE Conference and Exhibition incorporating SPE EUROPEC 2008, 2008
GPR permits to map over large the thickness and density of snow pack: these parameters are required when the snow water equivalent has to be estimated. The results of GPR , conducted on a slope in the Alps in Northern Italy, are discussed. The data acquisition along several profiles was repeated in different period of the winter season.
A. Godio, Godio A.
openaire   +4 more sources

Snow water equivalent variability and forecast in Lithuania

, 2002
Atmosphere circulation is the most important modulator of snow cover parameters. This study deals with the relation between the dominant Northern Hemisphere circulation mode, called the Arctic Oscillation (AO), and the spatial distribution of the snow water equivalent (SWE) within the territory of Lithuania.
Rimkus, E., Stankunavichius, G.
openaire   +2 more sources

Some of the next articles are maybe not open access.

Related searches:

Retrieval of Snow Water Equivalent by Gamma

IGARSS 2019 - 2019 IEEE International Geoscience and Remote Sensing Symposium, 2019
Snow cover can attenuate gamma rays in soil, take advantage of this property, the surface snow water equivalent over a large range can be measured more accurately, and it has the advantage of not destroying the surface characteristics. Considering the disturbance of soil moisture to the measurement results and the geographical characteristics of the ...
Yuan Ma, Hongyi Li 0003, Jian Wang 0032, Xiaohua Hao   +3 more
openaire   +1 more source

InSAR for estimation of changes in snow water equivalent of dry snow

IGARSS 2000. IEEE 2000 International Geoscience and Remote Sensing Symposium. Taking the Pulse of the Planet: The Role of Remote Sensing in Managing the Environment. Proceedings (Cat. No.00CH37120), 2001
This paper describes the theoretical relation between interferometric phase and changes in snow water equivalent (SWE) and show results from experiments using ERS- 1/2 tandem data. The main scattering contribution from a dry snow cover is from the snow-ground interface. However, the radar wave will be refracted in the snow.
Tore Guneriussen, Kjell Arild Høgda, Harald Johnsen, Inge Lauknes   +3 more
openaire   +1 more source

Snow Depth and Snow Water Equivalent Estimation

2021
Variation in regional and global snowfall significantly affects the ecological and climate systems, which is usually used for policy-making in water resource management and disaster prevention. The amount of snowfall is measured by two different parameters, snow depth and snow water equivalent (SWE). SWE is defined as the product of snow depth and snow
openaire   +1 more source