Livros: "Ground Weta"

1

Johns, P. M. Distribution and conservation status of ground weta, Hemiandrus species (Orthoptera:Anostostomatidae). Wellington, N.Z: Dept. of Conservation, 2001.

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2

Mackintosh, Robin. Wet wet wet special. London: Grandreams Limited, 1989.

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3

Hurr, R. Theodore. Estimating pumping time and ground-water withdrawals using energy-consumption data. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1990.

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4

Hurr, R. Theodore. Estimating pumping time and ground-water withdrawals using energy-consumption data. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1990.

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5

Hurr, R. Theodore. Estimating pumping time and ground-water withdrawals using energy-consumption data. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1990.

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6

Buyalski, Clark P. Gravel pack thickness for ground-water wells: Report no. 1. Denver, Colo: Hydraulics Branch, Division of Research and Laboratory Services, Engineering and Research Center, U.S. Dept. of the Interior, Bureau of Reclamation, 1986.

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7

Buyalski, Clark P. Gravel pack thickness for ground-water wells: Report no. 1. Denver, Colo: Hydraulics Branch, Division of Research and Laboratory Services, Engineering and Research Center, U.S. Dept. of the Interior, Bureau of Reclamation, 1986.

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8

Mal, Peachey, ed. Wet Wet Wet pictured. London: Virgin, 1995.

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9

Grannemann, N. G. Hydrogeology and ground-water quality of the Bay Mills Indian Community study area, near Brimley, Michigan. [Washington, D.C.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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10

Grannemann, N. G. Hydrogeology and ground-water quality of the Bay Mills Indian Community study area, near Brimley, Michigan. [Washington, D.C.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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11

Grannemann, N. G. Hydrogeology and ground-water quality of the Bay Mills Indian Community study area, near Brimley, Michigan. [Washington, D.C.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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12

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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13

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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14

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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15

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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16

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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17

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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18

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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19

Lacombe, Pierre. Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000. West Trenton, N.J: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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20

Hendriks, Aart. Wet gelijke behandeling op grond van handicap of chronische ziekte. Deventer: Kluwer, 2003.

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21

M. M. van der Burg. Wet gelijke behandeling op grond van leeftijd bij de arbeid. Deventer: Kluwer, 2004.

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22

Bos, Willem, e Daniël de Jongh. Op welke grond rust deze wet?: Beschouwingen over de Europese Grondwet. Amsterdam: Van Gennep, 2005.

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23

Drongelen, J. van. Wet gelijke behandeling op grond van leeftijd bij de arbeid: Tekst en toelichting. Den Haag: Sdu Uitgevers, 2004.

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24

Senyk, J. P. Ground-based wet weather yarding operations in coastal British Columbia: Effects on soil properties and seedling growth. Victoria, B.C: Pacific Forestry Centre, 1997.

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25

Senyk, J. P. Ground-based wet weather yarding operations in coastal British Columbia: Effects on soil properties and seedling growth. Victoria, B.C: Pacific Forestry Centre, 1997.

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26

(Netherlands), Emancipatieraad. Vier jaar Emancipatieraad: Onderzoek naar de taakvervulling op grond van artikel 12 van de Wet op de Emancipatieraad. Den Haag: De Raad, 1985.

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27

Peachey, Mal, e Simon Fowler. Wet Wet Wet: Pictured. Virgin Pub, 1996.

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28

Proposed work plan for the study of hydrologic effects of ground-water development in the Wet Mountain Valley, Colorado. Denver, Colo: U.S. Dept. of the Interior, Geological Survey, 1985.

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29

(Netherlands), Emancipatieraad, ed. Estafette, onderzoek naar de taakvervulling op grond van artikel 12 van de Wet op de Emancipatieraad: Mei 1985-mei 1989. Den Haag: Emancipatieraad, 1989.

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30

Erika, De Wet. Military Assistance on Request and the Use of Force. Oxford University Press, 2020. http://dx.doi.org/10.1093/law/9780198784401.001.0001.

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The book examines if and to what extent the proliferation of direct military assistance on the request of a recognized government is changing the rules regulating the use of force. Since the end of the Cold War, several (sub)regional organizations in Africa have codified military assistance on request in their respective treaty frameworks. In addition, in countries such as Afghanistan, Iraq, Libya, Mali, Somalia, South Sudan, Syria, and Yemen, internationally recognized governments embroiled in protracted armed conflicts have requested direct military assistance from individual states or groups of states. These requests are often accepted by the other states and at times the United Nations Security Council, even when the requesting governments have very limited effective control over their territories, lack democratic legitimacy and are engaged in wide-spread and systematic violations of international human rights and humanitarian law.This book departs from a definition of requested military assistance that refers to the exercise of forcible measures by third-state armed forces or those controlled by an international organization in the territory of the requesting state. It then examines the authority to issue a request for (or consent to) direct military assistance, as well as the type of situations in which such assistance may be requested—notably whether it can be requested during an armed conflict. De Wet finishes by examining the important and controversial question of whether and to what extent the proliferation of forcible assistance on request is changing the legal framework applying to the use of force in international law.

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31

Gao, Yanhong, e Deliang Chen. Modeling of Regional Climate over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.591.

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The modeling of climate over the Tibetan Plateau (TP) started with the introduction of Global Climate Models (GCMs) in the 1950s. Since then, GCMs have been developed to simulate atmospheric dynamics and eventually the climate system. As the highest and widest international plateau, the strong orographic forcing caused by the TP and its impact on general circulation rather than regional climate was initially the focus. Later, with growing awareness of the incapability of GCMs to depict regional or local-scale atmospheric processes over the heterogeneous ground, coupled with the importance of this information for local decision-making, regional climate models (RCMs) were established in the 1970s. Dynamic and thermodynamic influences of the TP on the East and South Asia summer monsoon have since been widely investigated by model. Besides the heterogeneity in topography, impacts of land cover heterogeneity and change on regional climate were widely modeled through sensitivity experiments.In recent decades, the TP has experienced a greater warming than the global average and those for similar latitudes. GCMs project a global pattern where the wet gets wetter and the dry gets drier. The climate regime over the TP covers the extreme arid regions from the northwest to the semi-humid region in the southeast. The increased warming over the TP compared to the global average raises a number of questions. What are the regional dryness/wetness changes over the TP? What is the mechanism of the responses of regional changes to global warming? To answer these questions, several dynamical downscaling models (DDMs) using RCMs focusing on the TP have recently been conducted and high-resolution data sets generated. All DDM studies demonstrated that this process-based approach, despite its limitations, can improve understandings of the processes that lead to precipitation on the TP. Observation and global land data assimilation systems both present more wetting in the northwestern arid/semi-arid regions than the southeastern humid/semi-humid regions. The DDM was found to better capture the observed elevation dependent warming over the TP. In addition, the long-term high-resolution climate simulation was found to better capture the spatial pattern of precipitation and P-E (precipitation minus evapotranspiration) changes than the best available global reanalysis. This facilitates new and substantial findings regarding the role of dynamical, thermodynamics, and transient eddies in P-E changes reflected in observed changes in major river basins fed by runoff from the TP. The DDM was found to add value regarding snowfall retrieval, precipitation frequency, and orographic precipitation.Although these advantages in the DDM over the TP are evidenced, there are unavoidable facts to be aware of. Firstly, there are still many discrepancies that exist in the up-to-date models. Any uncertainty in the model’s physics or in the land information from remote sensing and the forcing could result in uncertainties in simulation results. Secondly, the question remains of what is the appropriate resolution for resolving the TP’s heterogeneity. Thirdly, it is a challenge to include human activities in the climate models, although this is deemed necessary for future earth science. All-embracing further efforts are expected to improve regional climate models over the TP.

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