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  • Sea Level Rise — IPCC
    The Intergovernmental Panel on Climate Change (IPCC) is active socially – choose your network: Engage with the IPCC There are many ways to be involved and participate in the IPCC world
  • Special Report on the Ocean and Cryosphere in a Changing Climate - IPCC
    Global mean sea level (GMSL) is rising (virtually certain 1) and accelerating (high confidence 2) The sum of glacier and ice sheet contributions is now the dominant source of GMSL rise (very high confidence) GMSL from tide gauges and altimetry observations increased from 1 4 mm yr –1 over the period 1901–1990 to 2 1 mm yr –1 over the period 1970–2015 to 3 2 mm yr –1 over the period
  • Headline Statements — Special Report on the Ocean and . . . - IPCC
    B3 Sea level continues to rise at an increasing rate Extreme sea level events that are historically rare (once per century in the recent past) are projected to occur frequently (at least once per year) at many locations by 2050 in all RCP scenarios, especially in tropical regions (high confidence)
  • Summary for Policymakers - IPCC
    This Synthesis Report (SYR) of the IPCC Sixth Assessment Report (AR6) summarises the state of knowledge of climate change, its widespread impacts and risks, and climate change mitigation and adaptation global mean sea level will rise by about 2–3 m if warming is limited to 1 5°C and 2–6 m if limited to 2°C (>50%) by 2100 without
  • Chapter 9: Ocean, Cryosphere and Sea Level Change
    Global mean sea level change (Sections 9 6 and 2 3 3 3) is the change in volume of the ocean divided by the ocean surface area It is the sum of changes in ocean density (‘global mean thermosteric sea level change’) and changes in the ocean mass as a result of changes in the cryosphere or land-water storage (‘barystatic sea level change’)
  • Technical Summary — Special Report on the Ocean and Cryosphere . . . - IPCC
    This Technical Summary of the IPCC Special Report on Ocean and Cryosphere in a Changing Climate Beyond 2100, sea level will continue to rise for centuries due to continuing deep ocean heat uptake and mass loss of the GIS and AIS and will remain 4 2 3 1 1, 4 2 3 1 2, 4 2 3 6} Sea level rise is not globally uniform and varies regionally
  • Chapter 4: Sea Level Rise and Implications for Low-Lying Islands . . . - IPCC
    Global mean sea level (GMSL) is rising (virtually certain 1) and accelerating (high confidence 2) The sum of glacier and ice sheet contributions is now the dominant source of GMSL rise (very high confidence) GMSL from tide gauges and altimetry observations increased from 1 4 mm yr –1 over the period 1901–1990 to 2 1 mm yr –1 over the period 1970–2015 to 3 2 mm yr –1 over the period
  • Figure 4. 2 — Special Report on the Ocean and Cryosphere in a . . . - IPCC
    The two sets of two bars labelled B19 are from an expert elicitation for the Antarctic component (Bamber et al , 2019), and reflect the likely range for a 2oC and 5oC temperature warming (low confidence; details section 4 2 3 3 1) The bar labelled “prob ” indicates the likely range of a set of probabilistic projections (4 2 3 2)
  • FAQ Chapter 4 — Special Report on the Ocean and Cryosphere in a . . .
    Scientific evidence about sea level rise is clear: Global mean sea level rose by 1 5 mm per year during the period 1901–1990, accelerating to 3 6 mm per year during the period 2005–2015 It is likely to rise 0 61-1 10 m by 2100 if global greenhouse gas emissions are not mitigated (RCP8 5) However, a rise of 2 or more meters cannot be ruled
  • Fact sheet - Responding to Sea Level Rise - IPCC
    Sea level rise is already impacting ecosystems, human livelihoods, infrastructure, food security and climate mitigation at the coast and Risks to coastal cities and settlements are projected to increase by at least one order of magnitude by 2100 without significant adaptation and mitigation action (high confidence) {TS C 5 4} These risks
  • Chapter 4 | Climate Change 2021: The Physical Science Basis - IPCC
    Under the five scenarios assessed, it is virtually certain that global mean sea level (GMSL) will continue to rise through the 21st century For the period 2081–2100 relative to 1995–2014, GMSL is likely to rise by 0 46–0 74 m under SSP3-7 0 and by 0 30–0 54 m under SSP1-2 6 (medium confidence) For the assessment of change in GMSL, the
  • Chapter 2: High Mountain Areas — Special Report on the Ocean . . . - IPCC
    The projected global-scale relative mass losses 2015 – 2100 correspond to a sea level contribution of 94 (likely range 69 – 119) mm sea level equivalent (SLE) corresponding to an average rate of 1 1 (likely range 0 8 – 1 4) mm SLE yr-1 for RCP2 6, and 200 (likely range 156 to 240) mm SLE, a rate of 2 4 (likely range 1 8 – 2 8) mm SLE yr





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