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| 1 | Discharge planning rounds to the bedside: a patient- and family- centered approach 显示文摘 | Wrobleski DM Joswiak ME Dunn DF | 2014 | Medsurg Nurs2014，23，2： | 1 |
| 2 | Factors limiting anaerobic performance in adolescent males with cystic fibrosis显示文摘 | Boas SR Joswiak ML Nixon PA Fulton JA Orenstein DM | | 0，，： | 1 |
| 3 | A 70-yr record of oxygen-18 variability in an ice core from the Tanggula Mountains, central Tibetan Plateau显示文摘 | Joswiak D. R. Yao T. Wu G. Xu B. Zheng W | 2010 | Climate of the Past2010，，30： | 1 |
| 4 | Karyotypes of threespecies of the genus Phoxinus (Pisces:Cyprinidae)显示文摘 | JOSWIAK G R MOORE W S | 1980 | Copeia1980，，4： | 1 |
| 5 | Deposition ofanthropogenic aerosols in a southeastern Tibetan glacier 显示文摘 | Xu B Q Wang M Joswiak D R | 2009 | Journal of Geophysical Research2009，114，17： | 1 |
| 6 | Climatic and atmos- pheric circulation pattern variability from ice-core isotope/geo- chemistry records ( Altai, Tien Shan and Tibet)显示文摘 | Aizen V B Aizen E M Joswiak D R | 2006 | Annals of Glaciology2006，43，： | 1 |
| 7 | Effects of anaerobic exercise on the immune system in 8 to 17 year-old trained and untrained males显示文摘 | Boas SR Joswiak ML Bufalino K | 1995 | Med Sci Sport Exerc1995，27，： | 1 |
| 8 | Stable isotopic compositions of precipitation events from Kathmandu, southern slope of the Himalayas显示文摘Investigation of temporal variations in the stable d18 O and d D isotopes from Kathmandu's precipitation events shows that the relatively enriched d18 O and d D values in the winter(the dry season, dominated by the westerlies) were positively correlated with temperature,indicating a temperature effect controlling the changes of d18 O and d D. However, the d18 O and d D values were depleted in the summer(the wet season, dominated by the Indian monsoon), which were negatively correlated with precipitation amount, indicating an amount effect. In addition, the comparison of stable isotopes in precipitation from Kathmandu and Mawlong(near the Bay of Bengal)shows that the overall trends of d18 O and d D values at Kathmandu generally approximate those at Mawlong.However, there remain many differences between the details of the isotopic changes at Kathmandu versus those at Mawlong. Compared with those at Mawlong, the further rainout effect and the more intense lift effect of the oceanic moisture by the high mountains resulted in the moredepleted d18 O and d D values in summer precipitation at Kathmandu. A deuterium excess and the local meteoric water lines reveal that evaporation at Kathmandu exceeds that at Mawlong. The data also show that the Indian monsoon activities at Mawlong are more intense than those at Kathmandu. | Tek Bahadur Chhetri Tandong Yao Wusheng Yu Li Ding Daniel Joswiak Lide Tian Lochan Prasad Devkota Dongmei Qu | 2014 | Chinese Science Bulletin2014，59，34： | 0 |
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